Rocks geol
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Gneissic rock forms from metamorphism. Metamorphism changes the form, mineralogy, texture, and sometimes chemical composition of rocks through heat, pressure, and chemically active fluids. Gneissic rock has a banded appearance due to foliation and does not split easily. Quartz is another metamorphic rock that forms from sandstone and is very hard with fused quartz grains. Sedimentary rocks cover about 75% of land and ocean floors, forming from particles of eroded material transported and deposited by water, wind, glaciers or mass movement.
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Wacke ( graywacke)
Graywacke, also known as wacke, is a type of sandstone that is composed of sand mixed with mud. It forms in deep ocean waters through turbidity currents and submarine landslides that rapidly transport sediment short distances. Graywacke contains a higher percentage of clay and less rounded grains than typical sandstone. It displays graded bedding from larger grains settling out first during deposition from turbidity events. Fossils can occasionally be found that provide clues about the depositional environment.
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Graywacke, also known as wacke, is a type of sandstone that forms in deep marine environments from sediment transported short distances by turbidity currents. It is dark in color and composed of poorly sorted grains of quartz, feldspar and lithic fragments in a muddy matrix. Graywacke forms distinctive beds deposited by turbidity events, with grain size decreasing upwards due to settling from higher to lower energy during an event. Fossils are sometimes found in the shale layers between beds.
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1) Gneissic rock is a common type of metamorphic rock that forms from heat and pressure. It has a banded appearance due to light and dark minerals.
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Petroleum geology lab 1
Rocks are a combination of minerals that are bonded together in some way.
All rocks are made of minerals
Monomineralic- contain one mineral
Polymineralic- contain more than one mineral
Rocks are classified into three groups by how they are formed
Igneous Rocks
Sedimentary rock
Metamorphic rock
Metamorphic rocks
Metamorphic rocks are formed from existing rock types that have been altered by heat, pressure, and chemical processes usually while buried deep underground. There are two basic types - foliated rocks that have a banded or layered appearance due to heat and pressure, and non-foliated rocks that do not have distinct layers. Some common metamorphic rocks include gneiss, slate, schist, quartzite, and marble.
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This document provides information on different types of rocks:
1. It classifies rocks into three main categories - igneous, sedimentary, and metamorphic rocks.
2. Igneous rocks form from cooling magma and include intrusive rocks like granite and gabbro, and extrusive rocks like basalt.
3. Sedimentary rocks form through the compaction and cementation of sediments and include sandstone, limestone, shale, and conglomerate.
4. Metamorphic rocks form from existing rocks undergoing changes due to heat and pressure, transforming the rock material, and include quartzite, marble, and slate.
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This document discusses the geology of Coalinga, California. [1] Coalinga is known for its oil fields, drills, and coal mining. [2] The valley was originally below sea level and submerged, allowing various sediments and minerals to accumulate. [3] Later, uplift of the Coast Ranges enclosed the valley, and faulting filled it with sediments, creating a flat landscape just above sea level.
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The document discusses different types of rocks:
1. Igneous rocks form from cooling magma and include intrusive granitic rocks, extrusive volcanic rocks like basalt, and hypabyssal rocks.
2. Sedimentary rocks form through the lithification of sediments and include clastic rocks like sandstone, chemical rocks like limestone, and organic rocks like coal.
3. Metamorphic rocks form from the alteration of existing rocks under heat, pressure, and fluids, changing their texture and minerals. Foliated rocks include schist and gneiss, while non-foliated rocks include marble and quartzite.
Vein deposits of tin and tungsten.pptx
Vein deposits form when fractures in host rock are filled with minerals deposited by circulating aqueous solutions. Tungsten and tin deposits commonly occur as veins, stockworks, skarns and placers associated with granitic rocks. Tungsten veins and stockworks contain wolframite and scheelite within quartz veins in granites. Tungsten skarn deposits form at contacts between intrusions and other rocks. Tin occurs in pegmatite veins, cassiterite-quartz veins and stockworks, and cassiterite-sulphide veins associated with granites. Placer deposits of cassiterite provide an important source of tin.
Rocks Geology ppt.pdf
This document defines rocks and describes the three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from existing rocks undergoing changes due to heat and pressure in the Earth. Rocks can change between these types through geological processes in the rock cycle.
Metamorphism and metamorphic rocks ppt
This document discusses metamorphism and metamorphic rocks. Metamorphic rocks form from existing igneous, sedimentary, or other metamorphic rocks through heat, pressure, and chemically reactive fluids. Metamorphism progresses incrementally and involves the growth of new minerals and deformation of existing ones. Metamorphism occurs in various settings like contact, regional, and burial metamorphism. Factors like heat, pressure, and fluids drive changes in mineralogy and texture. Metamorphic grade is indicated by index minerals and results in foliated and non-foliated rock types.
Different Types of Rocks and the processes involved in its formation,ppt
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This document provides an overview of geology and exploration methods for petroleum. It discusses the three main rock types - igneous, sedimentary and metamorphic rocks - and describes parameters that control petroleum occurrence such as source rocks, reservoir rocks and traps. It then explains processes of petroleum migration and entrapment. Finally, it outlines various oil exploration methods including surface geology, geophysical techniques like magnetic, gravity and seismic surveys, and sub-surface methods like well correlation.
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The document provides an overview of geology and exploration methods for petroleum. It discusses the three main rock types - igneous, sedimentary and metamorphic rocks - and describes parameters that control petroleum occurrence such as source rocks, reservoir rocks and traps. It then explains processes of petroleum migration and entrapment. Finally, it outlines various oil exploration methods including surface geology, geophysical techniques like magnetic, gravity and seismic surveys, and sub-surface methods like well correlation.
Formation of rocks
Rocks form through three main processes: igneous, sedimentary, and metamorphic. Igneous rocks form when magma or lava cools and crystallizes. Sedimentary rocks form through the compaction and cementation of sediments over time. Metamorphic rocks were originally igneous or sedimentary rocks that were subjected to heat and pressure within the Earth, transforming their composition and structure.
Characteristics of sedimentary rocks
The document provides information about sedimentary rocks, including their formation, classification, characteristics, and types. It discusses how sedimentary rocks form through the compaction and cementation of sediments. It classifies sedimentary rocks based on the nature of sediments (mechanically, chemically, or organically formed) and transporting agents (aqueous, aeolian, glacial). It provides details on specific sedimentary rock types like sandstones, conglomerates, limestone, and their properties. The document also covers concepts like bedding, stratification, unconformities in sedimentary rocks.
Rocks Science..232323232323232323
This document defines and describes the three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma or lava. Sedimentary rocks form through the compaction or cementation of sediments. Metamorphic rocks form from existing rocks undergoing changes due to heat and pressure in the Earth. Rocks can change between these types through geological processes in the rock cycle.
Types of metasomatism
This document discusses different types of metasomatism classified based on metasomatic processes and geological position. There are two main types of metasomatic processes - diffusional metasomatism which occurs through diffusion, and infiltrational metasomatism which occurs through the transfer of materials in solution. The geological positions discussed include autometasomatism near magmatic bodies, contact metasomatism at contacts between bodies, and regional metasomatism over large areas. Specific metasomatic rock types are also summarized like fenite, greisens, and skarns, which are important in studying ore deposits.
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Sediment characteristics.ppt
This document provides an overview of sedimentology and sedimentary processes. It defines sedimentology as the scientific study of sedimentary rocks and the processes involved in their formation. Various types of sedimentary rocks are described based on their composition, such as clastic rocks composed of fragments, carbonates precipitated from water, and evaporites formed from evaporated water. Common sedimentary structures and environments are also outlined, including alluvial fans, rivers, lakes, deltas, and marine settings. Principles of sedimentary rock formation like superposition and lateral continuity are explained. Methodologies for analyzing and classifying sediments and sedimentary rocks are presented.
ROCKS pdf.pdf
The document discusses the rock cycle and the three main types of rocks - igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling of magma, either underground to form intrusive igneous rocks or on the surface to form extrusive igneous rocks. Sedimentary rocks form through the weathering of existing rocks and the deposition of sediments. Metamorphic rocks form from heat and pressure altering existing rocks deep underground. The rock cycle describes how rocks continuously change from one type to another through geological processes.
rock lecture 1.pdf
The document provides information about rocks from a lecture on the topic. It defines what rocks are, how they form, and the three main types of rocks: igneous, sedimentary, and metamorphic. It discusses how igneous rocks form from cooling magma, sedimentary rocks form through the lithification of sediments, and metamorphic rocks form from changes to existing rocks through heat, pressure, and fluid activity. Examples of different rock types are also provided.
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Syllabus
Chapter-1
Introduction to objective, scope and outcome the subject
Chapter 2
Introduction: Scope and Specialization of Civil Engineering, Role of civil Engineer in Society, Impact of infrastructural development on economy of country.
Chapter 3
Surveying: Object Principles & Types of Surveying; Site Plans, Plans & Maps; Scales & Unit of different Measurements.
Linear Measurements: Instruments used. Linear Measurement by Tape, Ranging out Survey Lines and overcoming Obstructions; Measurements on sloping ground; Tape corrections, conventional symbols. Angular Measurements: Instruments used; Introduction to Compass Surveying, Bearings and Longitude & Latitude of a Line, Introduction to total station.
Levelling: Instrument used Object of levelling, Methods of levelling in brief, and Contour maps.
Chapter 4
Buildings: Selection of site for Buildings, Layout of Building Plan, Types of buildings, Plinth area, carpet area, floor space index, Introduction to building byelaws, concept of sun light & ventilation. Components of Buildings & their functions, Basic concept of R.C.C., Introduction to types of foundation
Chapter 5
Transportation: Introduction to Transportation Engineering; Traffic and Road Safety: Types and Characteristics of Various Modes of Transportation; Various Road Traffic Signs, Causes of Accidents and Road Safety Measures.
Chapter 6
Environmental Engineering: Environmental Pollution, Environmental Acts and Regulations, Functional Concepts of Ecology, Basics of Species, Biodiversity, Ecosystem, Hydrological Cycle; Chemical Cycles: Carbon, Nitrogen & Phosphorus; Energy Flow in Ecosystems.
Water Pollution: Water Quality standards, Introduction to Treatment & Disposal of Waste Water. Reuse and Saving of Water, Rain Water Harvesting. Solid Waste Management: Classification of Solid Waste, Collection, Transportation and Disposal of Solid. Recycling of Solid Waste: Energy Recovery, Sanitary Landfill, On-Site Sanitation. Air & Noise Pollution: Primary and Secondary air pollutants, Harmful effects of Air Pollution, Control of Air Pollution. . Noise Pollution Harmful Effects of noise pollution, control of noise pollution, Global warming & Climate Change, Ozone depletion, Greenhouse effect
Text Books:
1. Palancharmy, Basic Civil Engineering, McGraw Hill publishers.
2. Satheesh Gopi, Basic Civil Engineering, Pearson Publishers.
3. Ketki Rangwala Dalal, Essentials of Civil Engineering, Charotar Publishing House.
4. BCP, Surveying volume 1
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Rocks geol
- 2. Metamorphism Rock Gneissic • Gneissic rock come from the Metamorphism rock. • Metamorphism rock change the form. • The changes are in the mineralogy, texture, and sometimes the chimical composition of rocks • Metamorphism rocks takes place usually in elevates temperatures and pressures. • This rocks gradually changes until state of equilibrium with the new enviroment. • The Agents of metamorphims include heat, pressure, and chemically active fluids.
- 3. Gneissic • Gneissic rock is common and widely distributed type of rock. • The rocks with a banded appearence are call gneissic. • Foliated gneissic will not usually split as easily as slates and some schists. • This gneissic rock I found in Turlock. • The place was in my way to Turlock near to highway
- 4. Gneissic • I identify the rock for the texture because are a little dark biotite flakes and the light silicate minerals. • Given the rock a banded or layered appearance. • Gneissic is a foliated texture
- 5. Quartz • The Changes on Metamorphism rocks increased the density, change in size, reorientation of mineral grains • The transformation of low temperature minerals into high temperature minerals. • Metamorphism rocks can be broadly classified in foliation exhibited and to lesser extend on the chemical composition. • Quartz is a very hard metamorphism rock.
- 6. Quartz • The quartz is a non foliated texture • Fused quarts grains, massive, very hard • We can find this type of rock in the water or near to it. • The quarts are formed in sandstone. • Quartz formed under moderate to high grade and the grains in sandstone fuse together. • The quartz ridges are often bare or covered only with very thin layer of soil and a little vegetation.
- 7. I identify this rock because is near to the water in yosemite and this rock shows grains typical of a quarts and this rocks are white to gray.
- 8. Sedimentary Rocks • About 75 percent of the land areas are covered by sediments and sedimentary rocks. • Across the ocean floor the earth solid surface, virtually everything is covered by sediment. • This rocks are mostly located in mid ocean, water and at some volcanic areas. • The particles of the sedimentary rocks by accumulating is call sediment.
- 9. Sedimentary Rocks • The sediment are formed by weathering and erosion in a source area and then they are transported to the place of deposition by water, winds mass movement or glaciers • This group of rock provides geologists with much of the basic information they need to reconstruct the details of Earth history.