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Carbonate diagenesis and po...
Carbonate diagenesis is a subject of enormous complexity because of the basic chemical reactivity of carbonate minerals. These carbonate minerals react quickly with natural waters that either dissolve the carbonates, or precipitate new carbonates to bring the water into equilibrium with the host carbonate sediments and rocks. These rock-water interactions either create porosity by dissolution, or destroy porosity by the precipitation of carbonate cements into pore spaces. Carbonate Diagenesis and Porosity examines these important relationships in detail. This volume is published in co-ope
Monografía
monografia Rebiun19695675 https://catalogo.rebiun.org/rebiun/record/Rebiun19695675 m o d | cr -n--------- 890629s1989 ne a ob 001 0 eng d 89007717 1-281-79064-8 9786611790646 0-08-086960-2 UPVA 997186733603706 UAM 991008423107104211 UPM 991005505296604212 UCAR 991008503197404213 MiAaPQ MiAaPQ MiAaPQ eng 552.58 552/.58 Moore, Clyde H. Carbonate diagenesis and porosity electronic resource] Clyde H. Moore Amsterdam New York Elsevier New York, NY, U.S.A. Distributors for the U.S. and Canada, Elsevier Science Pub. Co. 1989 Amsterdam New York New York, NY, U.S.A. Amsterdam New York Elsevier New York, NY, U.S.A. Distributors for the U.S. and Canada, Elsevier Science Pub. Co. 1 online resource (351 p.) 1 online resource (351 p.) Text txt computer c online resource cr Developments in sedimentology 46 Description based upon print version of record Includes bibliography and index Front Cover; Carbonate Diagenesis and Porosity; Copyright Page; Contents; Preface; Chapter 1. The Nature of Carbonate Depositional Systems-Comparison of Carbonates and Siliciclastics; Introduction; Consequences of Biological Influences over Carbonate Sediments; Sedimentary Processes and Depositional Environments Common to Both Carbonates and Siliclastics; Carbonate Rock Classification; Sedimentation Style-The Ubiquitous Carbonate Shoaling Upward Sequence and Cyclicity; Carbonate Shelf Evolution-Response to Sea Level The Changing Nature of Carbonate Shelf Margins in Response to Global TectonicsConsequences of High Chemical Reactivity of Carbonates Relative to Siliclastics; Summary; Chapter 2. The Classification and Nature of Carbonate Porosity; Introduction; The Classification of Carbonate Porosity; The Nature of Primary Porosity in Modern Carbonate Sediments; Secondary Porosity; Summary; Chapter 3. Diagenetic Environments of Porosity Modification and Tools for Their Recognition in the Geologic Record; Introduction; The Diagenetic Environments of Porosity Modification Tools for the Recognition of Diagenetic Environments of Porosity Modification in the Geologic RecordSummary; Chapter 4. Normal Marine Diagenetic Environments; Introduction; Shallow Water Normal Marine Diagenetic Environments; Deep Marine Diagenetic Environments; Summary; Chapter 5. Evaporative Marine Diagenetic Environments; Introduction; The Marginal Marine Sabkha Diagenetic Environment; Marginal Marine Evaporative Lagoons and Basins (Reflux Dolomitization); Summary; Chapter 6. Introduction to Diagenesis in the Meteoric Environment; Introduction; Geochemical and Mineralogical Considerations SummaryChapter 7. Meteoric Diagenetic Environments; Introduction; The Vadose Diagenetic Environment as Developed in Metastable Carbonate Sequences; The Meteoric Diagenetic Environment in Mature. Mineralogically Stable Systems; Summary; Chapter 8. Dolomitization Associated With Meteoric and Mixed Meteoric and Marine Waters; Introduction; Summary; Chapter 9. Burial Diagenetic Environment; Introduction; The Burial Setting; Compaction; Burial Cementation; Subsurface Dissolution; Subsurface Dolomitization The Role of Early, Surficial Depositional and Diagenetic Processes Versus Burial Processes in Shaping Ultimate Porosity EvolutionPredicting Changes in Porosity with Depth; Summary; References; Index Carbonate diagenesis is a subject of enormous complexity because of the basic chemical reactivity of carbonate minerals. These carbonate minerals react quickly with natural waters that either dissolve the carbonates, or precipitate new carbonates to bring the water into equilibrium with the host carbonate sediments and rocks. These rock-water interactions either create porosity by dissolution, or destroy porosity by the precipitation of carbonate cements into pore spaces. Carbonate Diagenesis and Porosity examines these important relationships in detail. This volume is published in co-ope English Carbonate rocks Diagenesis Porosity Electronic books Oil & Gas Consultants International 0-444-87415-1 Developments in Sedimentology