The document provides an overview of the mineralography sample preparation process using Struers equipment and methods. It discusses sampling techniques using the Accutom-50 or Discoplan-TS to cut samples, lapping samples flat, grinding glass slides, cementing samples to glass slides, and cutting off excess material. The goal is to produce thin sections that are plane parallel without cracks or relief between phases for analysis under transmitted or reflected light microscopy.
All Igneous rock textures with examples in easy and simple way to understand and increase microscopic studies skills and the way to easily identify igneous rocks under polarized microscope.
1. Igneous rock textures are determined by the cooling rate of molten rock material. Rapid cooling results in small crystal size or glassy texture, while slow cooling allows larger crystals to form.
2. Textures include phaneritic (visible crystals), holocrystalline (well-developed crystals), porphyritic (large and small crystals), and trachytic (aligned plagioclase crystals indicating lava flow).
3. Features like crystal size, shape, and mutual grain relationships are used to classify textures as equigranular, inequigranular, intergranular, and others which provide information about the cooling and crystallization history.
This document discusses the characteristics of gabbro, a dark-colored igneous rock. It defines gabbro and describes its typical mineral composition and textures. Gabbro forms large intrusive bodies worldwide and has economic importance due to deposits of chromium, platinum, and other metals. Notable examples of large gabbro deposits discussed are the Bushveld Complex in South Africa and the Stillwater Complex in Montana.
Mica are a group of silicate minerals whose outstanding physical characteristic is that individual mica crystals can easily be split into extremely thin elastic plates. This characteristic is described as perfect basal cleavage. Mica is common in igneous and metamorphic rock and is occasionally found as small flakes in sedimentary rock. It is particularly prominent in many granites, pegmatites, and schists.
Base metal exploration Benue trough final - Steffen KalbskopfSteffen Kalbskopf
A November 2020 update on the Nigerian government initiative in lead zinc & barite exploration with structure, stratigraphy, geochemical and remote sensing survey results, plus drill follow up
This document discusses several optical properties of minerals including crystal morphology, cleavage, inclusions, color, relief, pleochroism, and twinkling. Crystal morphology refers to the shape minerals exhibit in different rock types such as tabular, prismatic, or anhedral. Cleavage is the presence of parallel cracks in minerals like mica but not quartz or garnet. Inclusions are materials trapped inside minerals during formation. Color is generated by selective absorption of different parts of the light spectrum. Relief and pleochroism help identify minerals under microscope. Twinkling is the shining appearance seen in minerals with different refractive indices.
Diagenesis refers to the physical, chemical, and biological changes that sediments undergo after deposition to form sedimentary rock. It can include compaction, cementation, replacement of minerals, and formation of new minerals. There are three main stages of diagenesis: syndiagenesis during sedimentation, anadiagenesis involving compaction and maturation, and epidigenesis during emergence before erosion. Common diagenetic processes in mudrocks include mechanical and chemical compaction, which reduce porosity, and the formation of authigenic minerals like calcite, illite, and kaolinite via replacement or precipitation. Clay minerals are important indicators in hydrocarbon exploration as they can provide information about tectonics, hydrocarbon generation
This document discusses igneous rock textures. It explains that texture refers to the size, shape, and arrangement of mineral grains in a rock. Cooling rate controls igneous rock texture, with rapid cooling resulting in fine-grained textures and slow cooling producing coarse-grained rocks. Extrusive igneous rocks like lava have fine-grained textures due to rapid surface cooling, while intrusive plutonic rocks exhibit a variety of coarse-grained textures due to slower cooling underground. Examples of different igneous rock textures are described, including aphanitic, porphyritic, vesicular, glassy, phaneritic, and pegmatitic.
All Igneous rock textures with examples in easy and simple way to understand and increase microscopic studies skills and the way to easily identify igneous rocks under polarized microscope.
1. Igneous rock textures are determined by the cooling rate of molten rock material. Rapid cooling results in small crystal size or glassy texture, while slow cooling allows larger crystals to form.
2. Textures include phaneritic (visible crystals), holocrystalline (well-developed crystals), porphyritic (large and small crystals), and trachytic (aligned plagioclase crystals indicating lava flow).
3. Features like crystal size, shape, and mutual grain relationships are used to classify textures as equigranular, inequigranular, intergranular, and others which provide information about the cooling and crystallization history.
This document discusses the characteristics of gabbro, a dark-colored igneous rock. It defines gabbro and describes its typical mineral composition and textures. Gabbro forms large intrusive bodies worldwide and has economic importance due to deposits of chromium, platinum, and other metals. Notable examples of large gabbro deposits discussed are the Bushveld Complex in South Africa and the Stillwater Complex in Montana.
Mica are a group of silicate minerals whose outstanding physical characteristic is that individual mica crystals can easily be split into extremely thin elastic plates. This characteristic is described as perfect basal cleavage. Mica is common in igneous and metamorphic rock and is occasionally found as small flakes in sedimentary rock. It is particularly prominent in many granites, pegmatites, and schists.
Base metal exploration Benue trough final - Steffen KalbskopfSteffen Kalbskopf
A November 2020 update on the Nigerian government initiative in lead zinc & barite exploration with structure, stratigraphy, geochemical and remote sensing survey results, plus drill follow up
This document discusses several optical properties of minerals including crystal morphology, cleavage, inclusions, color, relief, pleochroism, and twinkling. Crystal morphology refers to the shape minerals exhibit in different rock types such as tabular, prismatic, or anhedral. Cleavage is the presence of parallel cracks in minerals like mica but not quartz or garnet. Inclusions are materials trapped inside minerals during formation. Color is generated by selective absorption of different parts of the light spectrum. Relief and pleochroism help identify minerals under microscope. Twinkling is the shining appearance seen in minerals with different refractive indices.
Diagenesis refers to the physical, chemical, and biological changes that sediments undergo after deposition to form sedimentary rock. It can include compaction, cementation, replacement of minerals, and formation of new minerals. There are three main stages of diagenesis: syndiagenesis during sedimentation, anadiagenesis involving compaction and maturation, and epidigenesis during emergence before erosion. Common diagenetic processes in mudrocks include mechanical and chemical compaction, which reduce porosity, and the formation of authigenic minerals like calcite, illite, and kaolinite via replacement or precipitation. Clay minerals are important indicators in hydrocarbon exploration as they can provide information about tectonics, hydrocarbon generation
This document discusses igneous rock textures. It explains that texture refers to the size, shape, and arrangement of mineral grains in a rock. Cooling rate controls igneous rock texture, with rapid cooling resulting in fine-grained textures and slow cooling producing coarse-grained rocks. Extrusive igneous rocks like lava have fine-grained textures due to rapid surface cooling, while intrusive plutonic rocks exhibit a variety of coarse-grained textures due to slower cooling underground. Examples of different igneous rock textures are described, including aphanitic, porphyritic, vesicular, glassy, phaneritic, and pegmatitic.
Kimberlite is a potassic, ultrabasic igneous rock that forms vertical pipes and intrusions. It has a porphyritic texture with large crystals in a fine-grained matrix. Kimberlites originate deep in the Earth's mantle and erupt explosively to the surface due to their high gas content. They are classified into Groups I and II based on mineral assemblages and textures. Kimberlites occur in crater, diatreme, and hypabyssal facies and are economically important sources of diamonds. The Wajrakarur field in India contains diamondiferous kimberlite pipes.
This document discusses different types of folds that can form in the Earth's crust. It describes how folds are caused by plastic deformation from compressive forces acting under conditions of stress, pressure, temperature gradients. There are three main mechanisms of folding: flexural folding where both competent and incompetent beds are bent, shear folding which involves slip along fractures, and flow folding where rocks fold like a fluid at high temperatures and depths. Common fold types include anticlines, synclines, and monoclines. Folds can form from tectonic processes like horizontal compression or mantle convection, or from non-tectonic processes like hillside creep or collapse structures.
This document provides a summary of the porphyry copper deposit model. It describes porphyry copper deposits as large-scale hydrothermal systems centered on porphyritic intrusions. Key points include:
- Porphyry copper deposits form in arc settings and are associated with porphyritic intrusions emplaced at depths between 1-4 km.
- Deposits can extend laterally over 1-4 km and vertically over 1-2 km. They contain both hypogene copper-bearing sulfide minerals and supergene copper oxide and sulfate minerals.
- Deposits display hydrothermal alteration assemblages including potassic, phyllic, argillic, and propylitic zones
Minerals are naturally occurring inorganic solid substances with a defined chemical composition and crystal structure. There are over 4,900 known mineral species, with silicate minerals making up over 90% of the Earth's crust. Minerals form through crystallization as ions come together and atoms arrange themselves in an ordered pattern. They can crystallize from magma or other melts as they cool, or form through precipitation from fluids. The scientific study of minerals is called mineralogy, which examines their chemistry, crystal structure, physical properties, origins, classification, and distribution. Key physical properties used to identify minerals include color, streak, luster, hardness, cleavage, and fracture.
Sedimentary structures provide important information about the depositional environment and post-depositional changes to sedimentary rocks. Key structures discussed include beds and bedding planes, laminations, graded bedding indicating changes in grain size over time, cross-bedding reflecting currents, load casts and flame structures from density differences, sole structures on bed bases indicating erosion, and trace fossils providing evidence of organism behavior and helping determine correct bed orientations. Together, an understanding of these sedimentary structures allows reconstruction of the depositional environment and testing of the law of superposition.
This document discusses the geology and mineral resources of Myanmar. It provides background on the tectonic setting resulting from the collision of the Indian and Asian plates. It describes the major geological features of Myanmar including sedimentary basins, magmatic belts, and metamorphic belts. It also summarizes the country's major mineral provinces and key mineral deposits such as tin-tungsten, lead-zinc-silver, and jade. Maps are included showing the distribution of these major deposit types across Myanmar.
This document discusses clay mineralogy and types of clay minerals. It begins by explaining that clay particles are small in size and composed mainly of secondary minerals. It then describes the main types of clay minerals:
1. Silicate clays which are crystalline and composed of tetrahedral and octahedral layers including kaolinite, smectite, micas, vermiculite, and chlorite.
2. Sesquioxide/oxidic clays which are highly weathered ultimate products containing iron and aluminum.
3. Amorphous clays which are non-crystalline and include allophane and imogolite commonly found in volcanic ash.
The document explains the characteristics
This document discusses joints, which are fractures in rock where there has been no displacement of the rock on either side. It classifies joints based on their geometry and genesis. Geometrically, joints are classified as strike joints, dip joints, or oblique joints based on their orientation relative to the bedding of the rock. Genetically, joints are classified as tension joints, which form perpendicular to tensional forces, or shear joints, which form due to shearing stresses during folding or faulting. Examples of tension joints include columnar joints, mud cracks, sheet joints, and mural joints. The document discusses the formation and features of these different joint types and their presence in igneous, sedimentary, and metam
Este documento describe las características de las rocas ígneas, incluyendo su grado de cristalización, tamaño de los cristales, y si son rocas volcánicas u plutónicas. Las rocas volcánicas tienen una textura hipocristalina o vítrea y pueden contener huecos de gas. Las rocas plutónicas tienen una textura holocristalina debido a su lento enfriamiento en el interior de la Tierra, y ejemplos comunes incluyen el granito.
Garnet is a group of six silicate minerals that are isomorphous and never occur in pure form. They vary slightly in properties but can be indistinguishable without analysis. Garnets have the general formula X3Y2(SiO4)3 and consist of silicon tetrahedrons linked to distorted metal octahedrons, forming a cubic crystal structure. They commonly occur as dodecahedrons or trapezohedrons and vary in color from red to green to black. Garnets are used as abrasives, for water jet cutting, filtration, and as gemstones due to their variety of colors and hardness.
Minerals used in Refractories and ceramicPramoda Raj
The document discusses various mineral raw materials used in the ceramic industry in India. The principal materials are silica in the form of quartz and other minerals, and alumino-silicates like feldspars and clays. Major sources of silica are quartzite, sandstone and high silica sands. Important feldspar sources are pegmatites in Rajasthan, Bihar and Andhra Pradesh. Ball clays are found in Rajasthan and Gujarat while china clay deposits exist across India. Refractory materials include fireclay, quartz, dolomite, magnesite, serpentine, olivine and chromite. The document also provides details on the
This document discusses the importance of studying textures of ore deposits to understand their genesis. It describes various textures including: 1) magmatic ores with cumulus, intergranular, and exsolution textures; 2) hydrothermal ore deposits and skarns with replacement and open space filling textures identified by criteria like pseudomorphs and matching fracture walls; and 3) near-surface deposits with colloform textures like botryoidal aggregates and Liesegang rings formed from colloidal solutions. Understanding these textures provides insight into the formation processes, conditions, and evolution of different ore deposit types.
The document discusses skarn deposits, which are metallic deposits associated with skarn rocks formed by the chemical alteration of carbonate rocks like dolostone and limestone. It defines skarn and its classifications, discusses associated mineral deposits, and highlights potential occurrences in Nigeria. Specifically, it notes that the Younger Granites Complex and marble-bearing schist belts may host skarn occurrences in Nigeria rich in iron, copper, gold, and molybdenum deposits. The document also presents a case study of the Antamina copper-zinc skarn deposit in Peru to illustrate deposit geology and mineralization.
This document summarizes the stratigraphic sequence and geological formations observed in the Hazara area. It describes 14 formations from the Late Precambrian to Early Paleocene in age, including their lithology, contacts, fossils, and age. Key formations discussed include the Hazara Slate Formation, Samanasuk Limestone, Chichali Shale, Lumshiwal Sandstone, and Kawagarh Limestone. The document also lists structures observed in the field such as folds, faults, veins, and contacts between units.
The document discusses lean iron ore beneficiation in India. It notes that India has over 25 billion tonnes of iron ore resources but reserves are depleting rapidly due to increased demand. Lean iron ore beneficiation techniques are needed to upgrade low-grade ores and maximize resource recovery in an environmentally sustainable way. This includes exploring deeper reserves, jigging, washing, classification, grinding, gravity separation, and magnetic separation to produce saleable iron ore concentrates and minimize waste disposal.
This document provides information about three industrial minerals: kaolinite, kyanite, and sillimanite. It describes their crystal structures, physical properties, modes of formation and occurrence. The key points are:
- Kaolinite, kyanite and sillimanite are formed through weathering of rocks or high pressure/temperature metamorphism.
- India has major deposits of these minerals, with Kerala, West Bengal, Rajasthan and Jharkhand highlighted as important producers.
- The minerals have various industrial uses like in ceramics, cement, and refractory applications due to their heat resistant properties.
The document discusses the Western Dharwar Craton located in peninsular India. It is bounded by mobile belts and contains various rock groups like the Sargur, Bababudan, and Chitradurga groups. The oldest rocks are the Gorur gneisses dated to 3500-3600 million years ago. Younger granites and schist belts containing ultramafic and mafic rocks cut across the craton. The economic deposits in the area include magnesite, iron, chromium, vanadium, and copper-nickel ores. The craton shows increasing metamorphic grade from greenschist in the north to amphibolite and granulite facies in the south.
Dokumen tersebut membahas tentang pasir besi, mulai dari definisi, genesa terbentuknya, karakteristik, eksplorasi, penambangan, pengolahan, dan pemanfaatannya. Pasir besi merupakan mineral sedimen yang kaya akan besi dan memiliki sifat magnetik, terbentuk dari erupsi gunung berapi lalu terakumulasi di pantai. Indonesia kaya akan sumber daya pasir besi yang dapat dimanfaatkan untuk industri baja, semen,
03 01 01_45-(flasking and processing complete denture)Serag Amer
This document discusses the flasking process for fabricating complete dentures. It describes the materials and techniques used, including the compression molding process of investing the master cast and wax denture set-up in dental stone inside a denture flask. It also briefly covers microwave and injection molding processing techniques. The key steps of boil out, packing of acrylic, curing, deflasking, and remounting are outlined. Remounting allows correction of any occlusal errors from the processing.
Academic presentation prepared for the final professional of BDS. The presentation talks about casting and investing techniques used in the Conservative Dentistry and Endodontics.
Kimberlite is a potassic, ultrabasic igneous rock that forms vertical pipes and intrusions. It has a porphyritic texture with large crystals in a fine-grained matrix. Kimberlites originate deep in the Earth's mantle and erupt explosively to the surface due to their high gas content. They are classified into Groups I and II based on mineral assemblages and textures. Kimberlites occur in crater, diatreme, and hypabyssal facies and are economically important sources of diamonds. The Wajrakarur field in India contains diamondiferous kimberlite pipes.
This document discusses different types of folds that can form in the Earth's crust. It describes how folds are caused by plastic deformation from compressive forces acting under conditions of stress, pressure, temperature gradients. There are three main mechanisms of folding: flexural folding where both competent and incompetent beds are bent, shear folding which involves slip along fractures, and flow folding where rocks fold like a fluid at high temperatures and depths. Common fold types include anticlines, synclines, and monoclines. Folds can form from tectonic processes like horizontal compression or mantle convection, or from non-tectonic processes like hillside creep or collapse structures.
This document provides a summary of the porphyry copper deposit model. It describes porphyry copper deposits as large-scale hydrothermal systems centered on porphyritic intrusions. Key points include:
- Porphyry copper deposits form in arc settings and are associated with porphyritic intrusions emplaced at depths between 1-4 km.
- Deposits can extend laterally over 1-4 km and vertically over 1-2 km. They contain both hypogene copper-bearing sulfide minerals and supergene copper oxide and sulfate minerals.
- Deposits display hydrothermal alteration assemblages including potassic, phyllic, argillic, and propylitic zones
Minerals are naturally occurring inorganic solid substances with a defined chemical composition and crystal structure. There are over 4,900 known mineral species, with silicate minerals making up over 90% of the Earth's crust. Minerals form through crystallization as ions come together and atoms arrange themselves in an ordered pattern. They can crystallize from magma or other melts as they cool, or form through precipitation from fluids. The scientific study of minerals is called mineralogy, which examines their chemistry, crystal structure, physical properties, origins, classification, and distribution. Key physical properties used to identify minerals include color, streak, luster, hardness, cleavage, and fracture.
Sedimentary structures provide important information about the depositional environment and post-depositional changes to sedimentary rocks. Key structures discussed include beds and bedding planes, laminations, graded bedding indicating changes in grain size over time, cross-bedding reflecting currents, load casts and flame structures from density differences, sole structures on bed bases indicating erosion, and trace fossils providing evidence of organism behavior and helping determine correct bed orientations. Together, an understanding of these sedimentary structures allows reconstruction of the depositional environment and testing of the law of superposition.
This document discusses the geology and mineral resources of Myanmar. It provides background on the tectonic setting resulting from the collision of the Indian and Asian plates. It describes the major geological features of Myanmar including sedimentary basins, magmatic belts, and metamorphic belts. It also summarizes the country's major mineral provinces and key mineral deposits such as tin-tungsten, lead-zinc-silver, and jade. Maps are included showing the distribution of these major deposit types across Myanmar.
This document discusses clay mineralogy and types of clay minerals. It begins by explaining that clay particles are small in size and composed mainly of secondary minerals. It then describes the main types of clay minerals:
1. Silicate clays which are crystalline and composed of tetrahedral and octahedral layers including kaolinite, smectite, micas, vermiculite, and chlorite.
2. Sesquioxide/oxidic clays which are highly weathered ultimate products containing iron and aluminum.
3. Amorphous clays which are non-crystalline and include allophane and imogolite commonly found in volcanic ash.
The document explains the characteristics
This document discusses joints, which are fractures in rock where there has been no displacement of the rock on either side. It classifies joints based on their geometry and genesis. Geometrically, joints are classified as strike joints, dip joints, or oblique joints based on their orientation relative to the bedding of the rock. Genetically, joints are classified as tension joints, which form perpendicular to tensional forces, or shear joints, which form due to shearing stresses during folding or faulting. Examples of tension joints include columnar joints, mud cracks, sheet joints, and mural joints. The document discusses the formation and features of these different joint types and their presence in igneous, sedimentary, and metam
Este documento describe las características de las rocas ígneas, incluyendo su grado de cristalización, tamaño de los cristales, y si son rocas volcánicas u plutónicas. Las rocas volcánicas tienen una textura hipocristalina o vítrea y pueden contener huecos de gas. Las rocas plutónicas tienen una textura holocristalina debido a su lento enfriamiento en el interior de la Tierra, y ejemplos comunes incluyen el granito.
Garnet is a group of six silicate minerals that are isomorphous and never occur in pure form. They vary slightly in properties but can be indistinguishable without analysis. Garnets have the general formula X3Y2(SiO4)3 and consist of silicon tetrahedrons linked to distorted metal octahedrons, forming a cubic crystal structure. They commonly occur as dodecahedrons or trapezohedrons and vary in color from red to green to black. Garnets are used as abrasives, for water jet cutting, filtration, and as gemstones due to their variety of colors and hardness.
Minerals used in Refractories and ceramicPramoda Raj
The document discusses various mineral raw materials used in the ceramic industry in India. The principal materials are silica in the form of quartz and other minerals, and alumino-silicates like feldspars and clays. Major sources of silica are quartzite, sandstone and high silica sands. Important feldspar sources are pegmatites in Rajasthan, Bihar and Andhra Pradesh. Ball clays are found in Rajasthan and Gujarat while china clay deposits exist across India. Refractory materials include fireclay, quartz, dolomite, magnesite, serpentine, olivine and chromite. The document also provides details on the
This document discusses the importance of studying textures of ore deposits to understand their genesis. It describes various textures including: 1) magmatic ores with cumulus, intergranular, and exsolution textures; 2) hydrothermal ore deposits and skarns with replacement and open space filling textures identified by criteria like pseudomorphs and matching fracture walls; and 3) near-surface deposits with colloform textures like botryoidal aggregates and Liesegang rings formed from colloidal solutions. Understanding these textures provides insight into the formation processes, conditions, and evolution of different ore deposit types.
The document discusses skarn deposits, which are metallic deposits associated with skarn rocks formed by the chemical alteration of carbonate rocks like dolostone and limestone. It defines skarn and its classifications, discusses associated mineral deposits, and highlights potential occurrences in Nigeria. Specifically, it notes that the Younger Granites Complex and marble-bearing schist belts may host skarn occurrences in Nigeria rich in iron, copper, gold, and molybdenum deposits. The document also presents a case study of the Antamina copper-zinc skarn deposit in Peru to illustrate deposit geology and mineralization.
This document summarizes the stratigraphic sequence and geological formations observed in the Hazara area. It describes 14 formations from the Late Precambrian to Early Paleocene in age, including their lithology, contacts, fossils, and age. Key formations discussed include the Hazara Slate Formation, Samanasuk Limestone, Chichali Shale, Lumshiwal Sandstone, and Kawagarh Limestone. The document also lists structures observed in the field such as folds, faults, veins, and contacts between units.
The document discusses lean iron ore beneficiation in India. It notes that India has over 25 billion tonnes of iron ore resources but reserves are depleting rapidly due to increased demand. Lean iron ore beneficiation techniques are needed to upgrade low-grade ores and maximize resource recovery in an environmentally sustainable way. This includes exploring deeper reserves, jigging, washing, classification, grinding, gravity separation, and magnetic separation to produce saleable iron ore concentrates and minimize waste disposal.
This document provides information about three industrial minerals: kaolinite, kyanite, and sillimanite. It describes their crystal structures, physical properties, modes of formation and occurrence. The key points are:
- Kaolinite, kyanite and sillimanite are formed through weathering of rocks or high pressure/temperature metamorphism.
- India has major deposits of these minerals, with Kerala, West Bengal, Rajasthan and Jharkhand highlighted as important producers.
- The minerals have various industrial uses like in ceramics, cement, and refractory applications due to their heat resistant properties.
The document discusses the Western Dharwar Craton located in peninsular India. It is bounded by mobile belts and contains various rock groups like the Sargur, Bababudan, and Chitradurga groups. The oldest rocks are the Gorur gneisses dated to 3500-3600 million years ago. Younger granites and schist belts containing ultramafic and mafic rocks cut across the craton. The economic deposits in the area include magnesite, iron, chromium, vanadium, and copper-nickel ores. The craton shows increasing metamorphic grade from greenschist in the north to amphibolite and granulite facies in the south.
Dokumen tersebut membahas tentang pasir besi, mulai dari definisi, genesa terbentuknya, karakteristik, eksplorasi, penambangan, pengolahan, dan pemanfaatannya. Pasir besi merupakan mineral sedimen yang kaya akan besi dan memiliki sifat magnetik, terbentuk dari erupsi gunung berapi lalu terakumulasi di pantai. Indonesia kaya akan sumber daya pasir besi yang dapat dimanfaatkan untuk industri baja, semen,
03 01 01_45-(flasking and processing complete denture)Serag Amer
This document discusses the flasking process for fabricating complete dentures. It describes the materials and techniques used, including the compression molding process of investing the master cast and wax denture set-up in dental stone inside a denture flask. It also briefly covers microwave and injection molding processing techniques. The key steps of boil out, packing of acrylic, curing, deflasking, and remounting are outlined. Remounting allows correction of any occlusal errors from the processing.
Academic presentation prepared for the final professional of BDS. The presentation talks about casting and investing techniques used in the Conservative Dentistry and Endodontics.
A presentation on topic Plastics ceramics and glass processing, the all content based on GTU syllabus And ideal for gtu students. The PPT contains videos for clear understanding of concept.
Narcissus Quagliata developed a new technique for creating fluid glass lines in fused glass works called "light paintings". This was done using a small kiln called the "vitrigraph" designed by Rudi Gritsch. The vitrigraph allows glass to be melted and drawn into lines resembling brush strokes, combining the fluidity of painting with the vibrancy of light in glass. The document describes the construction and use of the vitrigraph kiln, including loading it with glass, recommended firing cycles, and tools that can be used to manipulate the hot glass and create different line effects.
This document summarizes the key steps in denture processing using compression molding technique:
1. A trial denture is prepared and disarticulated from the cast.
2. The cast and trial denture are invested in dental stone in a flask.
3. The wax is boiled out of the flask. Retention grooves are placed on the artificial teeth.
4. Acrylic resin is mixed, packed into the flask, cured, cooled, and deflasked to produce the final denture.
5. The denture is then finished and polished.
Business Presentation 1 - Launching a new productIVAN C.
Presentación comercial creada por Iván Corral para la empresa Onyx Solar. El motivo era el lanzamiento de un nuevo producto, el vidrio fotovoltaico de colores, cuyas características y usos se describen en la propia presentación.
INTRODUCTION- Removable partial denture: the replacement of missing teeth and supporting tissues with a prosthesis designed to be removed by the wearer-GPT.
Cast partial denture is a type of partial denture comprising a cast metal framework with acrylic resin prosthetic teeth.
Traditional acrylic partial dentures are less durable, retentive, and stronger than cast partial dentures.
Catalogo de preparacion de muestras mineralogicas
http://www.izasa.es/productos/instrumentacion-cientifica/control-de-calidad-industrial/materialografia/preparaciones-especiales/preparacion-muestras-mineralogicas/discoplan-ts.aspx
This document is a lab manual for experiments related to building materials. It provides procedures and instructions for 9 experiments:
1. Determining the normal consistency of cement.
2. Measuring the initial and final setting time of cement.
3. Testing the compressive strength of cement samples.
4. Finding the specific gravity of fine aggregate.
5. Analyzing the grain size distribution of fine aggregate using sieves.
6. Measuring the crushing value of coarse aggregate.
7. Determining the impact value of aggregate.
8. Testing the compressive strength of concrete cubes.
9. Additional aggregate testing experiments are also described.
The
This document is a lab manual that outlines procedures for testing building materials. It includes 9 experiments:
1. Determining the normal consistency of cement
2. Measuring the initial and final setting time of cement
3. Testing the compressive strength of cement samples cured for 3, 7, and 28 days
4. Finding the specific gravity of a fine aggregate sample
5. Analyzing the grain size distribution of fine aggregates
6. Measuring the crushing value and impact value of aggregate samples
7. Determining the compressive strength of concrete cubes
The document provides detailed instructions for setting up and performing each experiment, including lists of required equipment and steps for taking measurements, making observations, and calculating
This document is a lab manual for experiments related to building materials. It provides procedures and instructions for 9 experiments:
1. Determining the normal consistency of cement.
2. Measuring the initial and final setting time of cement.
3. Testing the compressive strength of cement samples.
4. Finding the specific gravity of fine aggregate.
5. Analyzing the grain size distribution of fine aggregate using sieves.
6. Measuring the crushing value of coarse aggregate.
7. Determining the impact value of aggregate.
8. Testing the compressive strength of concrete cubes.
9. Additional aggregate testing experiments are also described.
The
This document provides an overview of the casting process used in dentistry. It discusses the history of lost wax casting techniques dating back to the Bronze Age. The key steps of the casting procedure are described, including making the wax pattern, adding a sprue, investing in a refractory material, and burning out the wax prior to casting. Common casting defects are also outlined relating to distortion, discoloration, porosities and other issues. Causes of defects are correlated to specific steps in the procedure. Details are provided on factors that influence optimal wax pattern design, sprue design and investment selection and parameters.
The document discusses the process of casting in dentistry. It begins with an introduction defining casting and its objective in dentistry. It then covers the history of casting in dentistry from ancient times through modern developments. The basic steps of casting are outlined, including spruing, investing, burnout, casting, recovery and cleaning. Different materials used for sprue formers, crucible formers, casting rings and liners are described. The document provides details on investing, burnout, and high and low heat techniques for casting gold and other alloys.
WHAT IS PLASTIC?
A synthetic material made from a wide range of organic polymers such as polyethylene, PVC, nylon, etc., that can be molded into shape while soft, and then set into a rigid or slightly elastic form.
This document provides information on spruing and investing for fixed prosthodontics. It discusses attaching a sprue former to wax patterns, and describes the purpose and proper attachment technique. It also discusses investing materials and techniques, including the components and purposes of gypsum-bonded and phosphate-bonded investments. The document provides step-by-step instructions for the vacuum-mix, vacuum-pour technique of investing a single-tooth wax pattern using a gypsum-bonded investment.
This document discusses the process of dental casting. It begins by defining casting and listing the main steps: preparing the wax pattern, spruing, investing, burnout, casting, recovery, and finishing. It then provides details on each step, including preparing the wax pattern, sprue design and materials, investing techniques, burnout methods, and common casting defects like porosity and distortion. The document is intended as an overview and guide for the dental casting procedure.
The fixture used in cage at this time currently
gives 6 nailguns in one cycle.
This takes a lot of time to manufacture if the units
are more in quantity. Also bending occurs at the
tip of the nailguns due to load.
To resolve this problem, a new fixture is designed
which will give 10 nail guns at a time and reduce
the bend
This document discusses various techniques for dental impressions, including:
1. Techniques are categorized based on mouth position (open vs closed), pressure applied (positive, negative, selective), mixing technique (double mix, putty-wash, monophase), and tray used (custom vs stock).
2. The putty-wash technique involves injecting light-body material around a tooth preparation and seating a tray filled with heavy-body material over it to capture both materials.
3. The monophase or single-mix technique uses a medium-viscosity material both in a stock tray and syringe to reduce waste and time compared to custom trays.
The document provides details on the casting procedure for partial denture frameworks. It discusses the history of dental casting, surveying the master cast, preparing it through blockout and relief, duplicating the cast, investing and spruing the wax pattern, burnout, casting, finishing and polishing the framework. The casting procedure involves duplicating the prepared master cast, adding sprues to the wax pattern, investing it, eliminating the wax through burnout, injecting molten alloy into the mold through centrifugal force, then recovering, cleaning and finishing the cast framework.
Este documento discute los riesgos laborales y aspectos de bioseguridad en el trabajo arqueológico en Bolivia. Reconoce actividades que ponen en riesgo al personal como excavaciones, trabajo de laboratorio e inspección de colecciones. Propone lineamientos para minimizar riesgos biológicos mediante el uso de equipo de protección y la implementación de protocolos. También aborda la conservación preventiva para evitar el deterioro de colecciones arqueológicas. Finalmente, enfatiza la necesidad de mayor conocimiento sobre bioseguridad
Este manual proporciona las pautas para la implementación de un Sistema de Gestión de Seguridad y Salud en el Trabajo. Describe los objetivos, alcance, definiciones clave, requisitos legales y las etapas del sistema, incluyendo la política, organización, planificación, evaluación y mejora continua. El objetivo final es identificar y controlar los riesgos laborales para proteger la seguridad y salud de los trabajadores.
This document provides an overview and abstracts from the colloquium "Art on the Rocks: Engaging the Public and Professionals to Network for Rock Art Conservation" held in Namibia in April 2017. The colloquium aimed to explore ways to increase public awareness of rock art and develop effective management strategies through discussions between international participants. It featured presentations on various approaches to public outreach, community involvement, site management, and collaboration between countries. The colloquium took place over a week, with discussions held in Windhoek and visits to the rock art sites of Brandberg and Twyfelfontein.
El documento describe las características de la estructura del suelo y la granulometría. Explica las propiedades de los suelos en función de la cantidad de finos y agregados presentes, como la permeabilidad, estabilidad y compactabilidad. También define conceptos como sensibilidad, tixotropía y desagregación que son importantes para entender el comportamiento de los suelos.
Este documento presenta una guía para la exploración del subsuelo y la caracterización geotécnica del terreno para proyectos de ingeniería. Explica la importancia de realizar una evaluación geotécnica del terreno y describe varias formaciones superficiales comunes como escarpes rocosos, colinas saprolíticas, laderas en suelos residuales, vegas y llanuras aluviales, entre otras. También destaca la necesidad de generar información cuantitativa sobre las propiedades de los suelos y rocas a través de muest
Este estudio evaluó los efectos del control intensivo versus estándar de la glucosa en pacientes veteranos con diabetes tipo 2. 1791 pacientes fueron asignados aleatoriamente a recibir terapia intensiva (nivel de HbA1c objetivo <6.9%) o estándar (nivel objetivo <8.4%). Aunque el control intensivo logró una mejora significativa en los niveles de glucosa, no hubo diferencias significativas en los eventos cardiovasculares primarios o la mortalidad entre los grupos. Sin embargo, hubo más episodios de hipogluce
Este documento describe la geometalurgia y su importancia para la minería. La geometalurgia integra la geología y la metalurgia para clasificar los minerales según su comportamiento metalúrgico. Ayuda a mejorar la evaluación de recursos y la rentabilidad de proyectos mineros al considerar variables geológicas y metalúrgicas. La aplicación efectiva de la geometalurgia requiere educar a profesionales en geometalurgia para que puedan integrar diferentes disciplinas y mejorar la planificación y operaciones mineras.
La geometalurgia es una herramienta multidisciplinaria que integra información geológica, minera, metalúrgica y económica para optimizar los procesos de explotación y beneficio de minerales. No existen laboratorios en México que realicen este tipo de trabajo, pero la Universidad de Sonora cuenta con los especialistas y la infraestructura necesarios para ofrecer servicios de geometalurgia a la industria minera mexicana. Se propone conformar un equipo de la universidad para vincularse con la industria y desarroll
La Unión Europea ha acordado un paquete de sanciones contra Rusia por su invasión de Ucrania. Las sanciones incluyen restricciones a las importaciones de productos rusos clave como el acero y limitar el acceso de los bancos rusos a los mercados financieros de la UE. Los líderes de la UE esperan que las sanciones aumenten la presión económica sobre Rusia y la disuadan de continuar su agresión contra Ucrania.
This document discusses a study analyzing 16 stone anchors recovered from the west coast of India to determine their geological provenance. Thin section analysis, X-ray fluorescence, and scanning electron microscopy with energy-dispersive spectroscopy were used to identify the rock types. The anchors were found to be composed of various igneous and sedimentary rocks indigenous to the region, including granodiorite, dolerite, basalt, schist, calcareous sandstone, limestone, and sandstone. This suggests the anchors were sourced locally from rock formations in Gujarat, Goa, Karnataka, and Maharashtra for use in ancient and medieval maritime trade activities along the west coast of India.
Este documento describe el uso de la fluorescencia de rayos X (FRX) para caracterizar materiales arqueológicos como cerámica y obsidiana. Se analizaron muestras de dos sitios arqueológicos en México y se compararon con muestras geológicas para determinar su procedencia. Los resultados mostraron que la mayoría de la obsidiana provenía de los yacimientos de Pico de Orizaba y Paredón, y que la cerámica Atoyac Gris Fino podría tener un origen foráneo como Oaxaca
This study analyzed 45 bronze coins from ancient Judea spanning the 1st centuries BCE and CE using metallography, x-ray diffraction and x-ray fluorescence to understand the minting methods. The results suggest coins were usually struck while still hot after being poured into molds. During the Roman occupation, reheating of coin flans before striking became more common, indicating developing specialization in minting. X-ray fluorescence also revealed changes in lead levels consistent with surrounding regions. The higher striking temperatures and more uniform die use in the 1st century CE under Roman rule point to greater control and efficiency in coin production even as output increased.
Este documento es un manual técnico sobre aguas subterráneas publicado en 2012 por el Ministerio de Ganadería, Agricultura y Pesca de Uruguay (MGAP) y el Proyecto Producción Responsable (PPR). El manual fue escrito por los doctores María Paula Collazo y Jorge Montaño, e incluye 18 capítulos sobre temas como el ciclo hidrológico, acuíferos, calidad del agua subterránea, contaminación, captación, construcción y abandono de pozos, entre otros. El manual tiene como objetivo
Este documento presenta los siete capítulos de un libro sobre los principios y fundamentos de la hidrología superficial. El capítulo 1 introduce conceptos básicos como el ciclo hidrológico y los procesos hidrológicos. El capítulo 2 describe las cuencas hidrológicas y sus características. El capítulo 3 cubre los temas de precipitación, mientras que el capítulo 4 explica el escurrimiento. El capítulo 5 trata sobre la infiltración y el capítulo 6 sobre las relaciones entre lluvia y escurrimiento.
Este documento presenta un capítulo sobre la atmósfera y el ciclo hidrológico para estudiantes de ingeniería civil. Explica que el ciclo hidrológico describe los cambios que experimenta el agua entre los estados sólido, líquido y gaseoso, así como entre formas superficiales y subterráneas. También introduce conceptos clave de la hidrología como proyectos hidráulicos, recursos hidrológicos, y el papel del estado en el estudio e implementación de dichos proyectos. Finalmente, señ
El análisis químico de suelos arqueológicos, en especial el análisis de fósforo, puede proporcionar información sobre actividades humanas antiguas al quedar atrapado el fósforo de los desechos orgánicos en el suelo por siglos. El estudio encontró altos niveles de fósforo, calcio y estroncio en dos trincheras, indicando alta actividad humana en esas áreas, posiblemente como cocinas, áreas de almacenamiento o consumo de alimentos. El anális
Este documento presenta el Plan de Contingencia de la Región San Martín del Perú para la temporada de lluvias de 2013, con el objetivo de mejorar la preparación y respuesta ante desastres que amenacen la salud pública. La región experimenta fuertes lluvias e inundaciones entre octubre y abril que han causado daños en el pasado. El plan busca estimar riesgos, fortalecer la prevención y preparación, e implementar una respuesta oportuna para proteger vidas y la salud de la población.
Plan de contingencias por inundaciones en caso de lluviasJulio Cesar Sierra
El documento presenta un plan de contingencia en caso de inundaciones por lluvias que incluye que el personal y estudiantes deben refugiarse en los salones u otras áreas designadas. La brigada de emergencias evaluará los daños y reportará al comité de emergencias, quien dará instrucciones de evacuar, refugiarse o regresar a actividades normales según sea necesario para garantizar la seguridad de todos.
El documento describe el estado de abandono de una torre medieval catalogada como Bien de Interés Cultural ubicada en un parque natural con alto valor ecológico en Cádiz, España. Se propone estudiar las patologías de la torre, hacer recomendaciones para su conservación, y mejorar los mecanismos para difundirla teniendo en cuenta cómo ha cambiado el paisaje que la rodea.
Analisis de c orrelacion de geoquimica y tipos de ceramicaJulio Cesar Sierra
Este documento describe un estudio realizado en Almizaraque, España, donde se analizaron 71 fragmentos cerámicos de cuatro tipos diferentes a través de fluorescencia de rayos X para determinar la composición de las materias primas utilizadas y observar si existe correlación entre la composición geoquímica y la tipología arqueológica. Los resultados muestran que es posible establecer esta correlación aplicando análisis de componentes principales y análisis discriminante a los datos geoquímicos.
UNLOCKING HEALTHCARE 4.0: NAVIGATING CRITICAL SUCCESS FACTORS FOR EFFECTIVE I...amsjournal
The Fourth Industrial Revolution is transforming industries, including healthcare, by integrating digital,
physical, and biological technologies. This study examines the integration of 4.0 technologies into
healthcare, identifying success factors and challenges through interviews with 70 stakeholders from 33
countries. Healthcare is evolving significantly, with varied objectives across nations aiming to improve
population health. The study explores stakeholders' perceptions on critical success factors, identifying
challenges such as insufficiently trained personnel, organizational silos, and structural barriers to data
exchange. Facilitators for integration include cost reduction initiatives and interoperability policies.
Technologies like IoT, Big Data, AI, Machine Learning, and robotics enhance diagnostics, treatment
precision, and real-time monitoring, reducing errors and optimizing resource utilization. Automation
improves employee satisfaction and patient care, while Blockchain and telemedicine drive cost reductions.
Successful integration requires skilled professionals and supportive policies, promising efficient resource
use, lower error rates, and accelerated processes, leading to optimized global healthcare outcomes.
The CBC machine is a common diagnostic tool used by doctors to measure a patient's red blood cell count, white blood cell count and platelet count. The machine uses a small sample of the patient's blood, which is then placed into special tubes and analyzed. The results of the analysis are then displayed on a screen for the doctor to review. The CBC machine is an important tool for diagnosing various conditions, such as anemia, infection and leukemia. It can also help to monitor a patient's response to treatment.
Understanding Inductive Bias in Machine LearningSUTEJAS
This presentation explores the concept of inductive bias in machine learning. It explains how algorithms come with built-in assumptions and preferences that guide the learning process. You'll learn about the different types of inductive bias and how they can impact the performance and generalizability of machine learning models.
The presentation also covers the positive and negative aspects of inductive bias, along with strategies for mitigating potential drawbacks. We'll explore examples of how bias manifests in algorithms like neural networks and decision trees.
By understanding inductive bias, you can gain valuable insights into how machine learning models work and make informed decisions when building and deploying them.
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Medical image analysis has witnessed significant advancements with deep learning techniques. In the domain of brain tumor segmentation, the ability to
precisely delineate tumor boundaries from magnetic resonance imaging (MRI)
scans holds profound implications for diagnosis. This study presents an ensemble convolutional neural network (CNN) with transfer learning, integrating
the state-of-the-art Deeplabv3+ architecture with the ResNet18 backbone. The
model is rigorously trained and evaluated, exhibiting remarkable performance
metrics, including an impressive global accuracy of 99.286%, a high-class accuracy of 82.191%, a mean intersection over union (IoU) of 79.900%, a weighted
IoU of 98.620%, and a Boundary F1 (BF) score of 83.303%. Notably, a detailed comparative analysis with existing methods showcases the superiority of
our proposed model. These findings underscore the model’s competence in precise brain tumor localization, underscoring its potential to revolutionize medical
image analysis and enhance healthcare outcomes. This research paves the way
for future exploration and optimization of advanced CNN models in medical
imaging, emphasizing addressing false positives and resource efficiency.
KuberTENes Birthday Bash Guadalajara - K8sGPT first impressionsVictor Morales
K8sGPT is a tool that analyzes and diagnoses Kubernetes clusters. This presentation was used to share the requirements and dependencies to deploy K8sGPT in a local environment.
Introduction- e - waste – definition - sources of e-waste– hazardous substances in e-waste - effects of e-waste on environment and human health- need for e-waste management– e-waste handling rules - waste minimization techniques for managing e-waste – recycling of e-waste - disposal treatment methods of e- waste – mechanism of extraction of precious metal from leaching solution-global Scenario of E-waste – E-waste in India- case studies.
Comparative analysis between traditional aquaponics and reconstructed aquapon...bijceesjournal
The aquaponic system of planting is a method that does not require soil usage. It is a method that only needs water, fish, lava rocks (a substitute for soil), and plants. Aquaponic systems are sustainable and environmentally friendly. Its use not only helps to plant in small spaces but also helps reduce artificial chemical use and minimizes excess water use, as aquaponics consumes 90% less water than soil-based gardening. The study applied a descriptive and experimental design to assess and compare conventional and reconstructed aquaponic methods for reproducing tomatoes. The researchers created an observation checklist to determine the significant factors of the study. The study aims to determine the significant difference between traditional aquaponics and reconstructed aquaponics systems propagating tomatoes in terms of height, weight, girth, and number of fruits. The reconstructed aquaponics system’s higher growth yield results in a much more nourished crop than the traditional aquaponics system. It is superior in its number of fruits, height, weight, and girth measurement. Moreover, the reconstructed aquaponics system is proven to eliminate all the hindrances present in the traditional aquaponics system, which are overcrowding of fish, algae growth, pest problems, contaminated water, and dead fish.
ACEP Magazine edition 4th launched on 05.06.2024Rahul
This document provides information about the third edition of the magazine "Sthapatya" published by the Association of Civil Engineers (Practicing) Aurangabad. It includes messages from current and past presidents of ACEP, memories and photos from past ACEP events, information on life time achievement awards given by ACEP, and a technical article on concrete maintenance, repairs and strengthening. The document highlights activities of ACEP and provides a technical educational article for members.
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CHINA’S GEO-ECONOMIC OUTREACH IN CENTRAL ASIAN COUNTRIES AND FUTURE PROSPECTjpsjournal1
The rivalry between prominent international actors for dominance over Central Asia's hydrocarbon
reserves and the ancient silk trade route, along with China's diplomatic endeavours in the area, has been
referred to as the "New Great Game." This research centres on the power struggle, considering
geopolitical, geostrategic, and geoeconomic variables. Topics including trade, political hegemony, oil
politics, and conventional and nontraditional security are all explored and explained by the researcher.
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in Central Asia. This study adheres to the empirical epistemological method and has taken care of
objectivity. This study analyze primary and secondary research documents critically to elaborate role of
china’s geo economic outreach in central Asian countries and its future prospect. China is thriving in trade,
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Shanghai Cooperation Organisation and the Belt and Road Economic Initiative. According to this study,
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Cooperation Organisation and the Belt and Road Economic Initiative.
2. P t ti O iPresentation Overview
1. Intro Mineralography – preparation definition(s)
2. Equipment
3. Installation and use of Accutom-50
4. The Struers TS-Method – concentration on A-50
www.struers.com
3. MineralographyMineralography
Groups
Minerals: Geological, petrographical samples, ores
Derived products: Refractories ceramics glassDerived products: Refractories, ceramics, glass
Mixed minerals: Cement, concrete products, densits
Common Properties
Hard, brittle, porous large hardness difference and little adhesion between
phasesp
Common Preparation Problems
Material will easily break risk for pull outs great tendency of relief buildingMaterial will easily break, risk for pull-outs, great tendency of relief building
and sometimes also water sensitive.
www.struers.com
4. Sample T pesSample Types
1) Thin Sections (+ cover glass)
For transmitted light
Sample 25 µm
Glue 5µ
Cover slide
Glass slide
S l 25
Glue 5µ
Sample 25 µm
Glass slide
2) Polished Thin Sections
For transmitted & reflected light
3) P li h d S l
Sample
Embedding
Material
3) Polished Samples
For reflected light only
www.struers.com
5. MineralographyMineralography
Demands - true structure
To remove deformed layer from cuttingTo remove deformed layer from cutting.
To obtain a surface without cracks,
scratches and no pull-outs.
Get a smooth and plane surface
Free from relief between hard & soft
phasesphases.
Plane parallel surface
Reflective
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15. Installation - Discoplan-TSInstallation Discoplan TS
Mounting and aligning cup wheel
1 Group washers in equals hights1. Group washers in equals hights
2. Group 3 x 3
3. Screw cup wheel on
4 Align to perfection by means of4. Align to perfection by means of
the dial gauge and Allen screw
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16. Installation Discoplan TSInstallation - Discoplan-TS
Plane grind vacuum chucks
1 Draw with a pencil1. Draw with a pencil.
2. Grind until lines are removed.
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17. Installation – Accutom-50Installation – Accutom-50
Plane grind vacuum chucks
1. Draw with a pencil.
2. Grind until lines are removed.
www.struers.com
19. The Struers TS-Method®The Struers TS Method
The steps to a perfect Thin Section
1 Sampling1. Sampling
2. Cutting
4. Glass slide
6 Mounting sample onto glass slide
3. Lapping sample5. Grinding glass slides
6. Mounting sample onto glass slide
7. Cutting surplus of sample
8 Grinding of Thin Section
9. Lapping (BORTY)
8. Grinding of Thin Section
10. Polishing (TYNDS)
www.struers.com
11. Completion
20. 1 S li (Di l TS)1. Sampling (Discoplan-TS)
Sample size: max 70-100mm
Use a diamond cut-off wheel (20TRE)
• Will not be wedge-shaped
• Thinner layer of deformation
• More economical
Use the jig to cut one side flat
Cut the other side 90º
www.struers.com
21. 1 S li (Di l TS)1. Sampling (Discoplan-TS)
Safety guard
Thumb screw
Safety guard
Holder for large
rocks
Guide PlateGuide Plate
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22. 1 Sampling (Accutom 50)1. Sampling (Accutom-50)
Sample size: max 40 mm (limitation) – for larger
samples use Discotom-6/Labotom-5 with
vertical clamping
U di d ff h l (M0D10/M0D13)Use a diamond cut-off wheel (M0D10/M0D13)
• Will not be wedge-shaped
• Thinner layer of deformation
M i l• More economical
Use a suitable jig to cut one side flat
Make a drawing on the specimen
where to make a thin section
www.struers.com
23. 2 Cutting Sample2. Cutting Sample
On left side of Discoplan-TS
Cut sample manually to a size of 8 x 20 x 30 mm
(St t d d)(Struers standard)
Use jig (3 sizes of cut)j g ( )
Use low force at the end of cutting to avoid
breakoutsbreakouts
Alternatively: Use Accutom-50
(see next slide)
www.struers.com
24. 2 Cutting Sample using jig2. Cutting Sample – using jig
On left side of Discoplan-TS
Moveable stopMoveable stop
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25. 2 C tti S l (A t 50)2. Cutting Sample (Accutom-50)
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26. 3. Lapping of Sample3. Lapping of Sample
LaboPol-35/LaboForce-MI + cast iron disc
(GRICO)
Lap one side of the sample (to be adhered to
glass slide)glass slide)
Use square sample mover plate (FOTON)
Cast iron lapping disc + SiC powder mixed in
glycerol/water #220 & #1000
Tip: use only a small amount of SiC-
powder, a tip of a teaspoon.
www.struers.com
27. After lappingAfter lapping
Turn on the hotplate and set the temperature at 135-140°C.
Make sure the hotplate has a layer of paper or tin foil on it.
Set your sample on the hotplate for at least 10–15 minutes
(l if th l i(longer if the sample is
porous or soft) so that it is completely dry before coming into
contact with epoxy.
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30. 4 Glass Slides Requirements4. Glass Slides - Requirements
Thickness: 1300-1500 µm (1.3 - 1.5mm)
Size: 27 x 46 mm or 28 x 48 mm
Edges: Preferably ground or sandblasted
• (stress free and safer)
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31. 5. Grind Glass Slides5. Grind Glass Slides
On Discoplan-TS using Diamond cup-wheel
G i d l lid t l ( +/ 2 )Grind glass slides to planeness (accuracy +/- 2 μm)
Use diamond cup wheel 01TYN.
Final Thickness:
1.164 for thin sections
1.150 for polished thin sections
www.struers.com
32. 5 Grind Glass Slides (size 1x3 inch)5. Grind Glass Slides (size 1x3 inch)
On Discoplan-TS using Diamond cup-wheel
www.struers.com
33. 5 Grind Glass Slides (Accutom 50)5. Grind Glass Slides (Accutom-50)
G i d l lid t l ( / 2 )Grind glass slides to planeness (accuracy +/- 2 μm)
Use diamond cup wheel .
Final Thickness – for use in BORTY:
1.164 for thin sections
1.150 for polished thin sections
www.struers.com
34. 5. Grind Glass Slides (Accutom-50)( )
- method set up -
www.struers.com
35. Gl Thi k ft G i diGlass Thickness after Grinding
Thin sections (with cover glass)
Glass 1.164 mm
Polished Thin sections
• Glass 1.150 mm
Epoxy 0.005
Thin section 0.025
“underlapping” 0.010
• Epoxy 0.005
• Thin section* 0.039
• “underlapping” 0.010
TOTAL thickness 1.204 • TOTAL thickness 1.204
* Before polishing
Sample 25 µm
Glue
Cover slide
Sample 39 µm
Glue
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Glass slide Glass slide
37. Gl Thi k ft G i di A t 50Glass Thickness after Grinding Accutom-50
Thin sections (with cover glass)
Glass 1.300 mm
Polished Thin sections
• Glass 1.300 mm
Epoxy 0.005
Thin section 0.025
“underlapping” 0.010
• Epoxy 0.005
• Thin section* 0.039
• “underlapping” 0.010
TOTAL thickness 1.340 • TOTAL thickness 1.354
* Before polishing
Sample 25 µm
Glue
Cover slide
Sample 39 µm
Glue
www.struers.com
Glass slide Glass slide
38. 6 Cementing Sample to Glass Slide6. Cementing Sample to Glass Slide
Use vacuum impregnation unit, Epovac + Epoxy.
Clean & dry samples thoroughly before mountingClean & dry samples thoroughly before mounting.
Cement the lapped side of sample to ground side of
glass slide.
Use Epovac and pressure rod to obtain extremely thinUse Epovac and pressure rod to obtain extremely thin
epoxy layer (5 μm).
www.struers.com
39. 6 Cementing Sample to Glass Slide6. Cementing Sample to Glass Slide
Use vacuum impregnation unit, CitoVac + Epoxy.
www.struers.com
40. 6 Cementing Sample to Glass Slide6. Cementing Sample to Glass Slide
• Turn on the hotplate and set the temperature at 35°C
• Make sure the hotplate has a layer of paper or foil on it.
• Set your sample on the hotplate for at least 10–15 minutesSet your sample on the hotplate for at least 10 15 minutes.
• Mix a batch of epoxy.
• When your sample is completely dry, get out a clean glass slide. Remove
your sample from the hotplate (careful, it will be hot!) and set it in front ofyour sample from the hotplate (careful, it will be hot!) and set it in front of
you with the face to be mounted pointed up.
• Place a small drop of epoxy on the surface of the sample and press a
clean glass slide onto the surface of the sample.g p
• You have a few minutes to position the glass, remove any bubbles, and/or
add additional epoxy before the epoxy begins to harden.
• To remove air bubbles, place a popsicle stick on the glass and slowly and
carefully “chase” the air bubbles to the edge of the sample by drawing
another popsicle stick from the middle of the sample to the edge.
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41. 6 Cementing Sample to Glass Slide6. Cementing Sample to Glass Slide
Once there are no more bubbles and the glass is properly centered, turn the sample
over and set it back on the hotplate at 80 C to cure with the glass slide up.
At this point you need to keep some pressure on the sample either with a weight orp y p p p g
with a pressure system on the hot plate.
All th t f i t l 45 i t d th l t it l ff thAllow the epoxy to cure for approximately 45 minutes, and then let it cool off the
hotplate for a while (time will vary depending on the sample) before handling it further.
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43. 6 Cementing Sample to Glass Slide6. Cementing Sample to Glass Slide
Let the sample cure with the glass slide
upwards and under a cupupwards and under a cup.
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44. 7 Cut-off Sample Surplus7. Cut off Sample Surplus
~ Re-sectioning
After Epoxy resin has cured, cut off
surplus material to a samplesurplus material to a sample
thickness of 0.5-1 mm
depending on the material.
Fix the sample on the vacuum
chuck at the left side of the
Discoplan TSDiscoplan-TS.
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47. 8. Grinding of Thin Sectiong
On Discoplan-TS using Diamond cup-wheel
G i d i di d h lGrind specimen on diamond cup-wheel
(01TYN) to a total thickness of approx. 80 μm
(section + resin)
Slide + sample + epoxy = 1.250 mm
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48. 8. Grinding of Thin Section8. Grinding of Thin Section
On Accutom-50 using Diamond cup-wheel
Grind specimen on diamond cup-wheel (M0P10 –
40 μm) to a total thickness of approx. 80 μm and
final grinding with M0P10 – 25 μm (section + resin)
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49. 9 Lapping of Thin section9. Lapping of Thin section
In BORTY on LaboPol-35 / LaboForce-MI
Lap sample (SiC powder #1000)
Use BORTY thin section holder
Lapping on a cast iron disc
Lap to desired thickness egLap to desired thickness eg.
• 25-30 µm for thin sections
• 30-35 μm for polished thin sections
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50. Microcover GlassMicrocover Glass
• Glue cover glass on by means of EUKITT
Cover slide
Sample 25 µm
Glue
Glass slide
Cover slide
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Glass slide
51. 10 Polishing in TYNDS10. Polishing in TYNDS
If polishing is required stop lapping or grinding with a sampleIf polishing is required, stop lapping or grinding with a sample
thickness of 30-35 μm as polishing removes further 5-10 µm.
SUse TYNDS thin section holder and polish.
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53. 11 Completed Sample11. Completed Sample
S l 30
Biotite
Sample 30 μm
Epoxy layer 5 μm
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54. 11 Completed Sample11. Completed Sample
S l 30
Metorite
Sample 30 μm
Epoxy layer 5 μm
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55. Polishing in TYNDSPolishing in TYNDS
Polishing the sample from 40µ down to required thickness
U TYNDS thi ti h ld d li hUse TYNDS thin section holder and polish.
Tegramin-30 / TegraSystem / LaboSystem - max 70 rpm
Time and force depends on the hardness of the material
Step
S f
Polishing 2Polishing1 Polishing 3
Surface
Abrasive
MD-Largo MD-Dac
DP-A DP-A
MD-Dac/Dur
DP-A
Grit /
grain size
Lubricant
6 µm 3 µm
Blue Blue
1 µm
Blue
[rpm]
Force
[N]
70 70
7.5 per sample 7.5 per sample
70
7.5 per sample
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Time
[min] 3-5 3-5 3-5
56. Polished thin section hard materialPolished thin section – hard material
Step Polishing 2Polishing1 Polishing 3Step
Surface
Polishing 2
MD-Largo MD-Pan/Dac MD-Dac/Dur
Polishing1 Polishing 3
Grit /
Abrasive DP-A DP-A DP-A
Grit /
grain size
Lubricant
9/6 µm 3 µm
Blue Blue
1 µm
Blue
[rpm] 70 70 70
Time
[min]
Force
[N] 10-15 per sample 10-15 per sample
3 5 3-5
10-15 per sample
3-5
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[min] 3-5 3 5 3 5
57. Polished thin section soft materialPolished thin section – soft material
Step Polishing 2Polishing1 Polishing 3Step
Surface
Polishing 2
MD-Pan MD-Dac MD-Dac/Dur
Polishing1 Polishing 3
Grit /
Abrasive DP-A DP-A DP-A
Grit /
grain size
Lubricant
6 µm 3 µm
Blue Blue
1 µm
Blue
[rpm] 70 70 70
Time
[min]
Force
[N] 5-10 per sample 5-10 per sample
3 5 3-5
5-10 per sample
3-5
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[min] 3-5 3 5 3 5
58. Lapping Cast Iron DiscLapping – Cast Iron Disc
Equipment: Discoplan-TS CitoVacEquipment: Discoplan-TS, CitoVac,
LaboPol-35/LaboForce-MI and accessories
#220: 80 ml powder + 1 liter
glycerine
#1000: 90 ml powder + 1 liter
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#1000: 90 ml powder + 1 liter
mixed glycerine/ water (1:3)
59. Polished thin section new methodPolished thin section – new method
E i t Di l TS Cit VEquipment: Discoplan-TS, CitoVac,
LaboPol-35/LaboForce-MI and accessories
#220: 80 ml powder + 1 liter glycerine
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#1000: 90 ml powder + 1 liter mixed glycerine/ water (1:3)
60. Polished thin section old methodPolished thin section – old method
Equipment: Discoplan-TS, CitoVac,
LaboPol-35/LaboForce-MI and accessories
#220: 80 ml powder + 1 liter glycerine
#1000 90 l d 1 lit i d l i / t (1 3)
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#1000: 90 ml powder + 1 liter mixed glycerine/ water (1:3)