Carbonate Facies in Geologic History

摘要: I Principles of Carbonate Sedimentation.- The Requisite Marine Environment: Warmth, Light, Water Movement.- Production Is Basically Organic.- Principal Hydrographic Controls on Accumulation.- Local Origin Particles-Textural Interpretation and Classification.- Deposition Rapid but Easily Inhibited Therefore Sporadic during Geologic Time.- Sediments Rock Are Peculiarly Subject to Many Stages Diagenesis.- Summary.- II Stratigraphy Deposits.- Definitions.- Basic Facies Pattern.- Paleotectonic Settings for Facies.- Stratigraphic Sequences, Geometry, Shelf Margins Basins.- Stratigraphie Sequences in Carbonates Epeiric Seas Shelves Shallow III Outline Petrography.- Techniques Examining Rocks.- Microfacies Interpretations.- Standard Types.- Diagenetic Changes Sediments.- Biological Observations.- Glossary Sedimentary Structures Environmental Analysis a Thin Section.- Significance Color Clastic Content Carbonates.- Porosity Permeability.- IV Advent Framebuilders the Middle Paleozoic.- Earliest Buildups.- Silurian Buildups - Settings.- Devonian V Lower Carboniferous Waulsortian Fades.- Relation Fades Regional Paleostructure.- Composition Typical Theories Mound Origin.- Condusions.- VI Pennsylvanian-Lower Permian Margin Southwestern United States America.- Setting, History, Climate.- Special Organic Communities Forming Late Paleozoic Strata.- Examples Permo-Pennsylvanian Conclusions.- VII Terrigenous-Carbonate Cycles.- Yoredale Pennsylvanian Wolfcampian Cyclothems Midcontinent Southern Rocky Mountains.- VIII Permo-Triassic Triassic Ecologic Reefs.- Reef Complex.- Dolomites.- Upper Reef-Lined Banks Basinal Mounds Austria Bavaria.- Similarities Differences between Complexes.- IX Trends Basin Deposits Jurassic Europe East.- Microfacies.- Girdle Central Europe.- Solnhofen X Shoaling upward Cycles Dolomitization.- Oolite-Grainstone Lime Mud-Sabkha Platform with Intense Dolomitization Interior XI Rise Rudists Cretaceous Mexico Rudist Bivalves.- Plattform-Bank Gulf Coast.- XII Principles.- Nine Belts an Ideal Model Three Major Types Profiles.- Associated Interrelations Parameters Controlling Modifying Accumulations.- Review Tectonic References.- Plates.