PDF-Journal of Sedimentary Research v

Author : tatyana-admore | Published Date : 2015-05-16

81 656669 Research Article DOI 102110jsr201151 USE OF CLUMPEDISOTOPE THERMOMETRY TO CONSTRAIN THE CRYSTALLIZATION TEMPERATURE OF DIAGENETIC CALCITE KATHARINE W HUNTINGTON

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Journal of Sedimentary Research v: Transcript


81 656669 Research Article DOI 102110jsr201151 USE OF CLUMPEDISOTOPE THERMOMETRY TO CONSTRAIN THE CRYSTALLIZATION TEMPERATURE OF DIAGENETIC CALCITE KATHARINE W HUNTINGTON DAVID A BUDD BRIAN P WERNICKE AND JOHN M EILER Department of Earth and. Sedimentary organic matter coal black shales oil gas brPage 2br Sedimentary organic matter verview coal black shales oil gas brPage 3br brPage 10br brPage 11br brPage 12br brP Sedimentary rocks cover ~ 75% of Earth’s surface. ~ 5 % (by volume) of Earth’s outer 10 miles. Contain evidence of past environments:. Important resource. Coal, oil, and other fossil fuels. Groundwater resources. Chemical Sedimentary Rocks. . Limestone. Chert – Silica. Evaporites. Organic Rocks. Coal. Oil and natural gas. Clastic Sedimentary Rocks. Formed from clasts (bits and pieces of pre-existing rocks) transported, deposited,and lithified. OR. Strategy:. Relate sedimentary characteristics of ancient deposits (grain size, . sedimentary . structures, geometry) to features observed in modern rivers. Bedforms. during traction deposition from unidirectional flow. Geology 103. Depositional environment. Is the term given to the area where the sediment was originally deposited. Must be inferred from the rock identity. Clastic. . depositional environments. Dominated by actions of waves, tides and currents. 2. TODAYS . MATERIAL:. Sedimentary . Rock and Sediment Description. Geologic Time. Sedimentary Environments. GEOL 332 Course Schedule. What is the Scientific Method?. What are the steps?. http://www.thwink.org/sustain/deadlock/WhyUnableToSolveProblem.htm. UNIT . 5. What are Sediments. Sediments are loose Earth materials (unconsolidated materials) such as sand . which are . transported by the action of water, wind, glacial ice and . gravity.. These . materials are . What is the difference between clastic and non-clastic sedimentary rocks? . What we know. The process of formation for a sedimentary rock involves the following steps:. Weathering. Erosion. Deposition. Favs. .. . Where do sediments come from?. - Weathering. – breaking down rock into smaller pieces chemically and physically.. - Erosion. - carrying away the particles and depositing them. . Glaciers. What are Sediments. Sediments are loose Earth materials (unconsolidated materials) such as sand . which are . transported by the action of water, wind, glacial ice and . gravity.. These . materials are . Sedimentary structures. Sedimentary structures.  are those structures formed during sediment deposition. .. Sedimentary structures such as . cross bedding, graded bedding, mud . cracks, . Strata. A rock is a natural substance that is made up of solid crystals of different minerals that have been fused together into a solid lump. . Rocks can be classified by their attributes: . Texture. Hardness. Sediment . Texture. Sediment texture refers to the shape, size and three-dimensional arrangement of the particles . that make . up sediment or a sedimentary rock.. Textures can be . clastic or . crystalline. Do Now. 1.  What is an igneous rock?. 2. How do sedimentary rocks form?. Sedimentary Rocks -. are one of the three main rock types . A sedimentary rock can form one of three ways: . by the . deposition.

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