What is Metamorphism and it's different aspects. What kind of metamorphisms take place at different tectonic regimes and their associate petro fabrics.
GRAPHIC QUARTZ-FELDSPAR INTERGROWTHS IN PEGMATITES: DIFFUSION AND GROWTH KINETICS MIGIF-HAFAFIT AREA, SOUTH EASTERN DESERT EGYPT
During the formation of pegmatites in the Migif-Hafafit area, conditions of crystallization were such that widespread graphic quartz-feldspar intergrowths were formed. The quartz is interpreted to have nucleated epinastically on rough edges and corners of alkali feldspar crystals. The existence of rugose inner feldspar-quartz boundaries and euhedral outer boundaries evidence that the graphic texture is a primary magmatic feature. Rapid growth, at or near volatile-saturated conditions, resulted in quartz saturation along the irregular melt-feldspar inner interface. Slow diffusion of Si and Al species (network formers) in the boundary-layer melt was likely the rate-controlling step for quartz saturation, which occurred along corners and edges, where the feldspar grew most rapidly. Diffusion-limited growth resulted in SiO2 buildup at the interface, producing oscillations from quartz-oversaturated to quartz-undersaturated conditions and thus the rhythmic quartz-feldspar intergrowths. The transition from planar, to edge, to cellular growth, and changes in the lobate inner feldspar-quartz boundary occurred in response to changes caused by crystallization that affect rates of Si-Al diffusion. Evidence of saturation in a volatile phase in these pegmatites indicates that water was a catalyst for feldspar growth and that lower activities of H2O in the melt decrease Si diffusivity at the crystal interface.
The Wadi Sikait Complex:
A Fertile- Post-Collisionl Granite-Pegmatite Suite, Eastern Desert, Egypt.
The Pan-African, Wadi Sikait Complex (WSC), in the south Eastern Desert of Egypt, is a late-tectonic, subsolvus strongly peraluminous, S-type, post-collisionl granite in the Sikait area that features an unambiguous genetic linkage with a proximal, zoned cluster of Be-, REE- and Nb-Ta bearing pegmatites (Abu Rusheid and Nugrus-Sikait area). The WSC is an arcuate belt of orthogneisses, migmatites and other high-grade metamorphic rocks, which mark the boundary between the central Eastern and the south Eastern Deserts of Egypt. The WSC consists of seven internal units (WSC-1 to -3 and PL-1 to -4) that range from chemically primitive biotite, garnet and sillimanite granites (WSC-1 and –2) to a highly evolved, tourmaline- and muscovite- bearing pegmatite granite facies (PL-1 to –4) locally containing endogenous emerald/beryl, molybdinite and cassiterite. Salient petrochemical attributes include A/CNK molar which varies from 1.15 to 1.75, a wide range of SiO2 (68.7-76.9%), high Al2O3 (14.1-16.0%), low CaO (<2.35%) and FeOt+MgO+TiO2 (0.36-6.62%), and with increasing fractionation, enrichment of Na2O, K2O, B, F, Be, Rb, Ga and Li, and depletion of Ba, Sr, Zr, REE and LREE. Strong fractionation is also revealed by Al/Ga (1370-6789), Ba/Rb (<0.01-12), Ca/Sr (21-201), K/Ba (19-9545), Mg/Li (4.26-1421), Na2O/K2O (0.21-34), (Ce/Yb)CN (0.89-83.25), and Eu/Eu* (<0.05-2.29). REE distribution patterns of rare-element pegmatites are lower in REE contents and flatter with prominent negative Eu anomaly than those of the related granites. The REE concentration and the (Ce/Yb)CN ratio decrease from the WSC-1 and -2 through PL-1 and -2 (fine-grained leucogranite) and PL-3 (pegmatitic leucogranite) to the PL-4 (potassic pegmatites).
Genesis of the strongly peraluminous, S-type granite and the associated rare-element pegmatite in the Sikait-Nugrus area is explained by a complex interplay of petrogenetic processes. Rare-elements and boron were previously concentrated in (wackes and mudstone) pelitic sediments deposited in large basins. These rocks underwent step-wise rock dehydration reactions involving muscovite and biotite, under fluid-absent conditions, and successively released these elements to anatectic melt. Rare-elements and volatiles were progressively concentrated via crystal-melt fractionation, the Harker trends of which were obscured by two stages of extraction of residual melt and by episodic, subsolidus redistribution via base-cation leaching. The late magmatic history of the WSC is marked by widespread exsolution of a volatile-rich phase, dispersion of a rare-element- F-B-Be-rich fluid along shear zones and ensuing emigration of rare-element-rich melt-fluid systems upward from the cupola, which led to the regionally zoned Sikait-Nugrus area
What is Metamorphism and it's different aspects. What kind of metamorphisms take place at different tectonic regimes and their associate petro fabrics.
GRAPHIC QUARTZ-FELDSPAR INTERGROWTHS IN PEGMATITES: DIFFUSION AND GROWTH KINETICS MIGIF-HAFAFIT AREA, SOUTH EASTERN DESERT EGYPT
During the formation of pegmatites in the Migif-Hafafit area, conditions of crystallization were such that widespread graphic quartz-feldspar intergrowths were formed. The quartz is interpreted to have nucleated epinastically on rough edges and corners of alkali feldspar crystals. The existence of rugose inner feldspar-quartz boundaries and euhedral outer boundaries evidence that the graphic texture is a primary magmatic feature. Rapid growth, at or near volatile-saturated conditions, resulted in quartz saturation along the irregular melt-feldspar inner interface. Slow diffusion of Si and Al species (network formers) in the boundary-layer melt was likely the rate-controlling step for quartz saturation, which occurred along corners and edges, where the feldspar grew most rapidly. Diffusion-limited growth resulted in SiO2 buildup at the interface, producing oscillations from quartz-oversaturated to quartz-undersaturated conditions and thus the rhythmic quartz-feldspar intergrowths. The transition from planar, to edge, to cellular growth, and changes in the lobate inner feldspar-quartz boundary occurred in response to changes caused by crystallization that affect rates of Si-Al diffusion. Evidence of saturation in a volatile phase in these pegmatites indicates that water was a catalyst for feldspar growth and that lower activities of H2O in the melt decrease Si diffusivity at the crystal interface.
The Wadi Sikait Complex:
A Fertile- Post-Collisionl Granite-Pegmatite Suite, Eastern Desert, Egypt.
The Pan-African, Wadi Sikait Complex (WSC), in the south Eastern Desert of Egypt, is a late-tectonic, subsolvus strongly peraluminous, S-type, post-collisionl granite in the Sikait area that features an unambiguous genetic linkage with a proximal, zoned cluster of Be-, REE- and Nb-Ta bearing pegmatites (Abu Rusheid and Nugrus-Sikait area). The WSC is an arcuate belt of orthogneisses, migmatites and other high-grade metamorphic rocks, which mark the boundary between the central Eastern and the south Eastern Deserts of Egypt. The WSC consists of seven internal units (WSC-1 to -3 and PL-1 to -4) that range from chemically primitive biotite, garnet and sillimanite granites (WSC-1 and –2) to a highly evolved, tourmaline- and muscovite- bearing pegmatite granite facies (PL-1 to –4) locally containing endogenous emerald/beryl, molybdinite and cassiterite. Salient petrochemical attributes include A/CNK molar which varies from 1.15 to 1.75, a wide range of SiO2 (68.7-76.9%), high Al2O3 (14.1-16.0%), low CaO (<2.35%) and FeOt+MgO+TiO2 (0.36-6.62%), and with increasing fractionation, enrichment of Na2O, K2O, B, F, Be, Rb, Ga and Li, and depletion of Ba, Sr, Zr, REE and LREE. Strong fractionation is also revealed by Al/Ga (1370-6789), Ba/Rb (<0.01-12), Ca/Sr (21-201), K/Ba (19-9545), Mg/Li (4.26-1421), Na2O/K2O (0.21-34), (Ce/Yb)CN (0.89-83.25), and Eu/Eu* (<0.05-2.29). REE distribution patterns of rare-element pegmatites are lower in REE contents and flatter with prominent negative Eu anomaly than those of the related granites. The REE concentration and the (Ce/Yb)CN ratio decrease from the WSC-1 and -2 through PL-1 and -2 (fine-grained leucogranite) and PL-3 (pegmatitic leucogranite) to the PL-4 (potassic pegmatites).
Genesis of the strongly peraluminous, S-type granite and the associated rare-element pegmatite in the Sikait-Nugrus area is explained by a complex interplay of petrogenetic processes. Rare-elements and boron were previously concentrated in (wackes and mudstone) pelitic sediments deposited in large basins. These rocks underwent step-wise rock dehydration reactions involving muscovite and biotite, under fluid-absent conditions, and successively released these elements to anatectic melt. Rare-elements and volatiles were progressively concentrated via crystal-melt fractionation, the Harker trends of which were obscured by two stages of extraction of residual melt and by episodic, subsolidus redistribution via base-cation leaching. The late magmatic history of the WSC is marked by widespread exsolution of a volatile-rich phase, dispersion of a rare-element- F-B-Be-rich fluid along shear zones and ensuing emigration of rare-element-rich melt-fluid systems upward from the cupola, which led to the regionally zoned Sikait-Nugrus area
Resource/reserve estimation depends first and foremost on a geological model that provides a sound, confident expectation that a well defined volume (deposit/domain) is mineralized throughout. Without this explicit decision regarding geological continuity of a delimited mineralized zone, neither estimates nor classification of mineral inventory is possible.
CONTINUITY; Geological Continuity; Value (Grade) Continuity; Primary factors that affect the estimation of value continuity; Continuity Domains; Reserves and Resources
PRIMARY GEOCHEMICAL HALOES IN PROSPECTING FOR GOLD DEPOSITS, UMM RUS MINE, EASTERN DESERT, EGYPT
The estimated Au values in the Umm Rus deposit are found to be dependent, besides physico-chemical factors, on the dip angles of the housing fractures and the amount of wedging-out of the quartz veins. The highest values are anticipated in the thin-gently dipping quartz veins which are commonly detected in some parts of level-279/ and level-487/. A stepwise discriminant analysis was used to reduce a number of potential pathfinder variables to an optimum group of pathfinder variables that differentiate between mineralized and unmineralized quartz vein samples.
The estimated Au values in the Umm Rus deposit are found to be dependent, besides physico-chemical factors, on the dip angles of the housing fractures and the amount of wedging-out of the quartz veins. The highest values are anticipated in the thin-gently dipping quartz vein
GOLD CONTENTS IN RELATION TO GEOMETRIC
FEATURES OF QUARTZ VEINS
Exploration in Deep Weathering Profiles, Supergene, R-mode factor analysis; Multi-element association geochemistry; Assessment of Au-Zn potentiality in Gossan; Rodruin-Egypt
Geological consultant, working in a range of roles from project development/feasibility study programs and advanced exploration roles. Contracts in a variety of global locations including Egypt, Saudi Arab, and the Middle East. Commodities including Gold, base metal sulfide, Gossan/Supergene, heavy mineral sands, clay/kaolin, Silica Sand, and iron ore.
Lithostratigraphic units Geology By Misson Choudhury Misson Choudhury
Misson Choudhury, Budding Geologists ,graduated from utkal university odisha,now pursuing M.sc applied geology in Bangalore university ..love to geologic mapping,drawing ,climbing ,tracking..
Reservoir types and Reservoir characterizations; Styles of Geologic Reservoir Heterogeneity; Classification of Heterogeneity; Scales of Geologic Reservoir Heterogeneity; Factors Causing Reservoir Heterogeneity; Assessing Reservoir Heterogeneity; Diagenetic and Reservoir Quality and Heterogeneity Implications in Deltaic and Marine Sandstones ; Scales of Fluvial Reservoir Heterogeneity; Impact of Bioturbation on Reservoir Heterogeneity; Carbonate Reservoir Heterogeneity
The palaeomagnetism of glauconitic sedimentsJohn Smith
The palaeoenvironmental significance of glaucony has long been appreciated, but accurate palaeomagnetic dating of events recorded by glauconitic horizons requires an understanding of how glauconitic sediments acquire a remanent magnetization. Pure glauconitic minerals are paramagnetic, but glauconite grains are large and slow-forming (over periods that can exceed 100 kyr), with complex and variable morphologies. It is, thus, possible that small magnetic grains within glaucony particles may carry a significant fraction of the remanence in weakly magnetized sediments. Any remanence carried by glauconitic grains may therefore represent the geomagnetic field at a time significantly later than the time of deposition, or a time-averaged signal over some or all of the formation period. We investigated this problem using weakly magnetic Palaeocene glauconitic siltstones from southern New Zealand. We disaggregated the rock and separated it magnetically into glauconitic and non-glauconitic fractions. Results from stepwise isothermal remanent magnetization (IRM) acquisition, alternating-field demagnetization, temperature dependence of magnetic susceptibility, and stepwise thermal demagnetization of a triaxial IRM were used to demonstrate that the remanent magnetization is carried by single-domain or pseudo-single-domain magnetite in the non-glauconitic sediment fraction, and that the glauconite grains themselves make no contribution to the remanent magnetization. However, accurate measurement of the primary remanence is complicated by a strong viscous overprint and mineral alteration during thermal demagnetization studies. Identification of magnetite as the remanence carrier in sediments within a reducing diagenetic environment gives confidence that the remanence has a depositional origin. Glauconite does not carry a remanence; therefore, its effect is to dilute and weaken the overall magnetization. Furthermore, the use of rock magnetic parameters may be problematic when glauconite concentrations are (as in the studied sediments) orders of magnitude greater than remanence carrier concentrations, because in such cases the glauconite susceptibility can dominate that of the remanence carriers.
Geological Time & Age Dating
Relative Time & Uniformitarianism
James Hutton & Kelvin
Law of Superposition
Lateral Continuity
Cross-Cutting Relationships
Fossil Succession
Law of Inclusions
Relative Age Dating
Absolute Age Dating
Fission-Track Dating
Carbon-14 dating
Tree-Ring dating
The Geologic Time Scale عمود الزمن الجيولوجى
Resource/reserve estimation depends first and foremost on a geological model that provides a sound, confident expectation that a well defined volume (deposit/domain) is mineralized throughout. Without this explicit decision regarding geological continuity of a delimited mineralized zone, neither estimates nor classification of mineral inventory is possible.
CONTINUITY; Geological Continuity; Value (Grade) Continuity; Primary factors that affect the estimation of value continuity; Continuity Domains; Reserves and Resources
PRIMARY GEOCHEMICAL HALOES IN PROSPECTING FOR GOLD DEPOSITS, UMM RUS MINE, EASTERN DESERT, EGYPT
The estimated Au values in the Umm Rus deposit are found to be dependent, besides physico-chemical factors, on the dip angles of the housing fractures and the amount of wedging-out of the quartz veins. The highest values are anticipated in the thin-gently dipping quartz veins which are commonly detected in some parts of level-279/ and level-487/. A stepwise discriminant analysis was used to reduce a number of potential pathfinder variables to an optimum group of pathfinder variables that differentiate between mineralized and unmineralized quartz vein samples.
The estimated Au values in the Umm Rus deposit are found to be dependent, besides physico-chemical factors, on the dip angles of the housing fractures and the amount of wedging-out of the quartz veins. The highest values are anticipated in the thin-gently dipping quartz vein
GOLD CONTENTS IN RELATION TO GEOMETRIC
FEATURES OF QUARTZ VEINS
Exploration in Deep Weathering Profiles, Supergene, R-mode factor analysis; Multi-element association geochemistry; Assessment of Au-Zn potentiality in Gossan; Rodruin-Egypt
Geological consultant, working in a range of roles from project development/feasibility study programs and advanced exploration roles. Contracts in a variety of global locations including Egypt, Saudi Arab, and the Middle East. Commodities including Gold, base metal sulfide, Gossan/Supergene, heavy mineral sands, clay/kaolin, Silica Sand, and iron ore.
Lithostratigraphic units Geology By Misson Choudhury Misson Choudhury
Misson Choudhury, Budding Geologists ,graduated from utkal university odisha,now pursuing M.sc applied geology in Bangalore university ..love to geologic mapping,drawing ,climbing ,tracking..
Reservoir types and Reservoir characterizations; Styles of Geologic Reservoir Heterogeneity; Classification of Heterogeneity; Scales of Geologic Reservoir Heterogeneity; Factors Causing Reservoir Heterogeneity; Assessing Reservoir Heterogeneity; Diagenetic and Reservoir Quality and Heterogeneity Implications in Deltaic and Marine Sandstones ; Scales of Fluvial Reservoir Heterogeneity; Impact of Bioturbation on Reservoir Heterogeneity; Carbonate Reservoir Heterogeneity
The palaeomagnetism of glauconitic sedimentsJohn Smith
The palaeoenvironmental significance of glaucony has long been appreciated, but accurate palaeomagnetic dating of events recorded by glauconitic horizons requires an understanding of how glauconitic sediments acquire a remanent magnetization. Pure glauconitic minerals are paramagnetic, but glauconite grains are large and slow-forming (over periods that can exceed 100 kyr), with complex and variable morphologies. It is, thus, possible that small magnetic grains within glaucony particles may carry a significant fraction of the remanence in weakly magnetized sediments. Any remanence carried by glauconitic grains may therefore represent the geomagnetic field at a time significantly later than the time of deposition, or a time-averaged signal over some or all of the formation period. We investigated this problem using weakly magnetic Palaeocene glauconitic siltstones from southern New Zealand. We disaggregated the rock and separated it magnetically into glauconitic and non-glauconitic fractions. Results from stepwise isothermal remanent magnetization (IRM) acquisition, alternating-field demagnetization, temperature dependence of magnetic susceptibility, and stepwise thermal demagnetization of a triaxial IRM were used to demonstrate that the remanent magnetization is carried by single-domain or pseudo-single-domain magnetite in the non-glauconitic sediment fraction, and that the glauconite grains themselves make no contribution to the remanent magnetization. However, accurate measurement of the primary remanence is complicated by a strong viscous overprint and mineral alteration during thermal demagnetization studies. Identification of magnetite as the remanence carrier in sediments within a reducing diagenetic environment gives confidence that the remanence has a depositional origin. Glauconite does not carry a remanence; therefore, its effect is to dilute and weaken the overall magnetization. Furthermore, the use of rock magnetic parameters may be problematic when glauconite concentrations are (as in the studied sediments) orders of magnitude greater than remanence carrier concentrations, because in such cases the glauconite susceptibility can dominate that of the remanence carriers.
Geological Time & Age Dating
Relative Time & Uniformitarianism
James Hutton & Kelvin
Law of Superposition
Lateral Continuity
Cross-Cutting Relationships
Fossil Succession
Law of Inclusions
Relative Age Dating
Absolute Age Dating
Fission-Track Dating
Carbon-14 dating
Tree-Ring dating
The Geologic Time Scale عمود الزمن الجيولوجى
Maria teresamaldonadosada unidad2actividad1May Sada
En esta presentación se presenta de manera detallada el tema de "Introducción a la Redacción de Artículos Científicos" como primera tarea de la Unidad 2 del Doctorado en Gestión y Transferencia del Conocimiento, donde encontrarás las diferencias de artículos científicos, las etapas que debe de tener un artículo científico y algunos tips para empezar las lecturas antes de desarrollar un artículo científico
La seguridad de recibir lo prometido debe estar basada en la fidelidad de Dios, y esta certeza, debe producir en nosotros un efecto esperanzador Estudio: Pastor Marino Estrella, Editado por: Olor a Gloria
Definition, metamorphism.
limits and type of metamorphic agents.
Metamorphic processes.
Types of Metamorphism
Classification of metamorphic rocks and textures of metamorphic rocks
Mineral assemblages and Metamorphic grade and facies of metamorphic rocks.
Graphic representation of metamorphic mineral parageneses.
Metamorphic Rocks ( Definition - Classification - Common Rocks ) Muhammad Mamdouh
presented for Dr | Magdy Basta
Faculty of petroleum and mining engineering, Suez University
Physical Geology Course ( 2016 - 2017 )
presented by : G7 - Members
Physical geology, petrology—sedimentary, igneous and metamorphic rocks. Basic principles of stratigraphy. Structural geology—faults, folds, joints, etc. Process of mineral formation. Classification of mineral deposits.
Linked in by ahmed al kawaliny | نصائح لبناء لينكيدإنAhmed Alkawaliny
Linked in by ahmed al kawaliny
Tips help you to build a good linkedIn
Thanks to Masr Ta3mal ^^
Moataz Yasser^^
**please Check SOBS Zag-Team on Facebook
- My linkedIn , Feel free to connect and write a recommendation ❤ :
https://eg.linkedin.com/in/ahmedalkawaliny
- prezi about me :
https://prezi.com/ukopsq9h6__3/a-few-things-about-me/
_____
other Contacts :
https://twitter.com/kawaliny
https://ask.fm/AhmedAbdoAlkawaliny
_____.
Cv Smart Tips by Ahmed Al-kawaliny
Tips help you to build a good CV
Thanks to Masr Ta3mal ^^
Moataz Yasser^^
**please Check SOBS Zag-Team on Facebook
- My linkedIn , Feel free to connect and write a recommendation ❤ :
https://eg.linkedin.com/in/ahmedalkawaliny
- prezi about me :
https://prezi.com/ukopsq9h6__3/a-few-things-about-me/
_____
other Contacts :
https://twitter.com/kawaliny
https://ask.fm/AhmedAbdoAlkawaliny
_____.
Weathering, erosion & soil
Introduction
Alteration of Minerals and Rocks
Mechanical Weathering
Frost Wedging
Pressure Release
Thermal Expansion and Contraction
Growth of Salt Crystals
Organisms
Organisms and Weathering
Chemical Weathering Decomposition of Earth Materials
Oxidation
Hydrolysis
Erosion
Sand Dunes
Expansive Soils and Soil Degradation
Weathering and Natural Resources
Soil and Its Origin
The Composition of Soil and Soil Horizons
Geological structures- التراكيب الجيولوجيه
Geological Structures
What are Geologic Structures?
إيه هيا التراكيب الجيولوجيه؟
Division of Structures
تقسيم للتراكيب الجيولوجيه
A- Primary structures
Ripple marks
Mud cracks
Cross bedding
Graded bedding
Burrows
B- Secondary Structures
Folds
Faults
Joints
Unconformities
What are Geologic Structures?
إيه هيا التراكيب الجيولوجيه؟
Geologic structure is any feature in rocks that results from deformation, such as folds, joints, and faults.
اى شكل فى الصخر ينتج من خلال عملية التشويه مثل : الصدوع والطيات
هى التشققات والتصدعات الضخمة والالتواءات العنيفة التى تشوه صخور القشرة الارضية .
Geologic structures are usually the result of the powerful tectonic forces that occur within the earth. These forces fold and break rocks, form deep faults, and build mountains .
Division of Structures
• Primary (or sedimentary) structures: such as ripple marks, cross-bedding, and mud cracks form in sediments during or shortly after deposition.
هى التراكيب الناتجة من تدخل العمليات الخارجية أثناء الترسيب
• Secondary structures: is that structures formed after the formations of any kind of rocks, such as folds, faults, or unconformities.
Primary structures
They are any structures in sedimentary rock formed at or shortly after the time of deposition: such as:
هى الاشكال التى تتخلف بالصخور تحت تأثير عوامل مناخية وبيئية خاصة مثل الجفاف والحرارة وتأثير الرياح والتيارات المائية وغيرها وبدون أى تدخل من جانب القوى والحركات الارضية أمثلة ذلك:
Ripple marks
علامات النيم: هي تموجات رملية صغيرة تنشأ على سطح الطبقات الرسوبية بواسطة حركة الماء أو الهواء و تكون حروف علامات النيم متعامدة على اتجاه الحركة.
They are wavelike (undulating) structures produced in granular sediment such as sand by unidirectional wind and water currents or by oscillating wave currents.
Wind and current ripples. (Asymmetric
Wave ripples. (Symmetric
Mud cracks
التشققات فى الرواسب الطينية : حيث ينكمش سطح الرسوبيات الطينية مخلفة شقوقا مميزة فى فترات الجفاف
Mud crack is a crack in clay-rich sediment that has dried out.
Cross bedding
التطبق المتقاطع هو النمط الذي تسلكه الرسوبيات الجديدة المتراكمة عند تأثرها بأي من التيارات المائية أو الهوائية. عندما تستق
Welcome to TechSoup New Member Orientation and Q&A (May 2024).pdfTechSoup
In this webinar you will learn how your organization can access TechSoup's wide variety of product discount and donation programs. From hardware to software, we'll give you a tour of the tools available to help your nonprofit with productivity, collaboration, financial management, donor tracking, security, and more.
Embracing GenAI - A Strategic ImperativePeter Windle
Artificial Intelligence (AI) technologies such as Generative AI, Image Generators and Large Language Models have had a dramatic impact on teaching, learning and assessment over the past 18 months. The most immediate threat AI posed was to Academic Integrity with Higher Education Institutes (HEIs) focusing their efforts on combating the use of GenAI in assessment. Guidelines were developed for staff and students, policies put in place too. Innovative educators have forged paths in the use of Generative AI for teaching, learning and assessments leading to pockets of transformation springing up across HEIs, often with little or no top-down guidance, support or direction.
This Gasta posits a strategic approach to integrating AI into HEIs to prepare staff, students and the curriculum for an evolving world and workplace. We will highlight the advantages of working with these technologies beyond the realm of teaching, learning and assessment by considering prompt engineering skills, industry impact, curriculum changes, and the need for staff upskilling. In contrast, not engaging strategically with Generative AI poses risks, including falling behind peers, missed opportunities and failing to ensure our graduates remain employable. The rapid evolution of AI technologies necessitates a proactive and strategic approach if we are to remain relevant.
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
Introduction to AI for Nonprofits with Tapp NetworkTechSoup
Dive into the world of AI! Experts Jon Hill and Tareq Monaur will guide you through AI's role in enhancing nonprofit websites and basic marketing strategies, making it easy to understand and apply.
The French Revolution, which began in 1789, was a period of radical social and political upheaval in France. It marked the decline of absolute monarchies, the rise of secular and democratic republics, and the eventual rise of Napoleon Bonaparte. This revolutionary period is crucial in understanding the transition from feudalism to modernity in Europe.
For more information, visit-www.vavaclasses.com
Francesca Gottschalk - How can education support child empowerment.pptxEduSkills OECD
Francesca Gottschalk from the OECD’s Centre for Educational Research and Innovation presents at the Ask an Expert Webinar: How can education support child empowerment?
Honest Reviews of Tim Han LMA Course Program.pptxtimhan337
Personal development courses are widely available today, with each one promising life-changing outcomes. Tim Han’s Life Mastery Achievers (LMA) Course has drawn a lot of interest. In addition to offering my frank assessment of Success Insider’s LMA Course, this piece examines the course’s effects via a variety of Tim Han LMA course reviews and Success Insider comments.
Operation “Blue Star” is the only event in the history of Independent India where the state went into war with its own people. Even after about 40 years it is not clear if it was culmination of states anger over people of the region, a political game of power or start of dictatorial chapter in the democratic setup.
The people of Punjab felt alienated from main stream due to denial of their just demands during a long democratic struggle since independence. As it happen all over the word, it led to militant struggle with great loss of lives of military, police and civilian personnel. Killing of Indira Gandhi and massacre of innocent Sikhs in Delhi and other India cities was also associated with this movement.
Metamorphic Rocks - lec" 7" - Geology for 1th year | Zagazig university.
1. Geology_______________________________________________________Metamorphic Rocks
Ahmed Al-kawaliny_ Senior Geologist at Zag Univ.
Head of SOBS ZAG Team.
Page | 1
Geology
Metamorphic Rocks
____________________
Outlines: _
Definition.
Features of metamorphism.
Agents / factors of metamorphism.
Types of metamorphism.
Textures of metamorphic Rocks.
ــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــــ
Definition:
Metamorphism – “a Greek word – Meta = Change,
Morph = Form.So, Metamorphism Means Change in
the Form. “
-= يصبح معناها وبذلك ، شكل : مورف ، تغيير تعنى : ميتا
. الشكل فى التغيير
2. Geology_______________________________________________________Metamorphic Rocks
Ahmed Al-kawaliny_ Senior Geologist at Zag Univ.
Head of SOBS ZAG Team.
Page | 2
Metamorphism : it’s recrystallization of pre-existing
rock under the effect of temperature , pressure or
chemically active fluids .
-الحرارة تأثير تحت سابقا موجود صخر من صخر تكوين إعادة
. الكيميائيه العوامل او والضغط
_____________________
Features of Metamorphism
1 – Metamorphism take place in the solid state
before melting.
2 – It can be considered to be iso-chemical except
for addition or removal of volatiles “ like water “
Or
It may cause extensive or strong change in
chemistry , So it’s called “ metasomatism “.
3. Geology_______________________________________________________Metamorphic Rocks
Ahmed Al-kawaliny_ Senior Geologist at Zag Univ.
Head of SOBS ZAG Team.
Page | 3
-؟ دا الكالم ايه يعنى
. التحول خصائص او مالمح
1-فى يحدث ال " . االنصهار قبل الصلبه الحاله فى يحدث
" االنصهار
2–ايزو " هو لذلك الكيميائيه العناصر تغييرفى او تبادل يحدث ال
" كيميائى–. الماء مثل المتطايرة المواد بعض اضافة باستثناء
بفعل للصخر الكيميائي التركيب فى شديد تبادل حدث إذا آخر بمعنى
" وليس " ميتاسوماتيزم " النوع هذا يسمى ، الكيميائيه العوامل
" ميتامورفيزم
Metasomatism:
change in the composition of a rock as a result of the
introduction or removal of chemical constituents.
4. Geology_______________________________________________________Metamorphic Rocks
Ahmed Al-kawaliny_ Senior Geologist at Zag Univ.
Head of SOBS ZAG Team.
Page | 4
Agents of Metamorphism .
1- Temperature.
2- Pressure.
3- Chemically active fluid.
_______________________
1- Temperature.
= Sources :-
a)Rising of magma bodies.
b)Geothermal Gradient.
c) Heat flow of mantle.
d)Rapid uplifting and erosion.
e)Radioactive Decay.
-: الحراره مصدر
a).الصهارة المادة صعود
b)بمعدل ، الحرارة زادت العمق زاد كلما : الحرارى التدرج
30درجه. متر كيلو لكل . س
c). الوشاح من المتدفقة الحرارة
5. Geology_______________________________________________________Metamorphic Rocks
Ahmed Al-kawaliny_ Senior Geologist at Zag Univ.
Head of SOBS ZAG Team.
Page | 5
d). التآكل و السريعه الرفع عمليات
e).االشعاعى " االضمحالل او االنحالل " التحلل
: الحظ
- Limits of temperatures
lower limit (150±50 °C)
higher limit (beginning of melting, 650-1100
°C)
ــــــــــــــــــــــــــــــــــــــــــ
2- Pressure : is define as force/unit area.
=Source :
a)Geogabric gradient : increase the pressure by
increasing depth “ 1k.bar / 3 Km “
b)Lithostatic Pressure : this pressure is uniform
in all directions by equal stresses acting on a
rock . – it doesn’t cause deformation.
c) Plate tectonic movement.
6. Geology_______________________________________________________Metamorphic Rocks
Ahmed Al-kawaliny_ Senior Geologist at Zag Univ.
Head of SOBS ZAG Team.
Page | 6
_________________
3- Fluids :
a)Spaces,pores and cracks are filled with
fluids.
b)Fluids make metamorphism more easily.
c) Fluids increase the rate if chemical reaction.
___________________________________________
Types of metamorphism:
They are related to agents of metamorphism which
are dominated, Predominant.
a)Dynamic Metamorphism = Cataclastic.
b)Thermal / Contact Metamorphism.
c) Regional Metamorphism.
7. Geology_______________________________________________________Metamorphic Rocks
Ahmed Al-kawaliny_ Senior Geologist at Zag Univ.
Head of SOBS ZAG Team.
Page | 7
Dynamic Metamorphism = Cataclastic.
- Pressure is the predominant agent.
- Produced from directive stress, occurs along the
fault zones or fault planes.
- This type cause crashing and granulation.
- EX : Mylonite.
Thermal / Contact Metamorphism.
Temperature is the main agent
Form as concentric zones (aureole) around hot
Igneous intrusive body . EX. Quartzite, Marble.
Textures of rocks that affected by contact
metamorphism known by:
- Overgrowth in crystals.
- Has no preferred orientation.
8. Geology_______________________________________________________Metamorphic Rocks
Ahmed Al-kawaliny_ Senior Geologist at Zag Univ.
Head of SOBS ZAG Team.
Page | 8
Regional Metamorphism.
Takes place in a very large area, related to high
temperature and pressure.
- Low grade of metamorphism. EX: slate .
- Medium: ex. Schist , Phyllite.
- High : ex. Gneiss,Migmatite.
____________________________________________
Textures of Metamorphic rocks :
1- Foliated
Rock has preferred orientation. due to effect of
pressure.
2- Non Foliated
Called Mosaic,Granoplastic or polygonal.
9. Geology_______________________________________________________Metamorphic Rocks
Ahmed Al-kawaliny_ Senior Geologist at Zag Univ.
Head of SOBS ZAG Team.
Page | 9
Foliated Metamorphic Rocks
• Slate
Dull, microscopic grains (could not seen by 10 x
lense), strong slaty cleavage, silky appearnce,
mudstone protolith
• Phyllite
Shiny, strongly micaceous with microscopic
grains (could seen by 10 x lense), strong
schistosity, cleavage, can be mafic or felsic, any
rock-type protolith.
Non-foliated Metamorphic rocks
Quartzite
• Metamorphosed sandstone
• Coarser and harder than the original
sandstones
10. Geology_______________________________________________________Metamorphic Rocks
Ahmed Al-kawaliny_ Senior Geologist at Zag Univ.
Head of SOBS ZAG Team.
Page | 10
• Harder than marble
• Will not release CO2 in the presence of acid
Marble
• Metamorphosed limestone “ calcite”
• Harder and coarser than the original
limestone
• Contains calcium carbonate
• Will release CO2 in the presence of acid
• Softer than quartzite