Descripción del título
Carbonate-clastic transitio...
Over the years, the field of sedimentology has become subdivided into various specialities. Two of the largest groups are those who study clastic rocks and those who study carbonates. There is little communication between the two: journals appear which are exclusively devoted to one or the other, and research conferences tend to be mutually exclusive. On the other hand, rocks themselves cannot be ""pigeon-holed"" in this way - the facies change from clastic to carbonate both laterally and through time. This volume stems from the editors' observations of such changes in the Gulf of Mexico a
Monografía
monografia Rebiun29254061 https://catalogo.rebiun.org/rebiun/record/Rebiun29254061 m o d | cr -n--------- 891004s1988 ne a ob 000 0 eng d 87030362 1-281-78124-X 9786611781248 0-08-086956-4 UPVA 997187637403706 MiAaPQ MiAaPQ MiAaPQ eng 552.5 552/.5 19 Carbonate-clastic transitions electronic resource] editors, Larry J. Doyle and Harry H. Roberts Amsterdam New York Elsevier 1988 Amsterdam New York Amsterdam New York Elsevier 1 online resource (313 p.) 1 online resource (313 p.) Text txt computer c online resource cr Developments in sedimentology 42 Description based upon print version of record Includes bibliographies Front Cover; Carbonate - Clastic Transitions; Copyright Page; Table of Contents; Preface; Chapter 1. Plate Tectonic Control of Global Patterns of Detrital and Carbonate Sedimentation; Chapter 2. Sedimentary Models of Siliciclastic Deposits and Coral Reef Interrelation; Chapter 3. Histories of Coexisting Reefs and Terrigenous Sediments: the Gulf of Elat (Red Sea), Java Sea, and Neogene Basin of the Negev, Israel; Chapter 4. Gulfs of Northern Red Sea: Depositional Settings of Distinct Siliciclastic-Carbonate Interfaces Chapter 5. Terrigenous and Carbonate Sedimentation in the Great Barrier Reef ProvinceChapter 6. Mixed Siliciclastic/Carbonate Sediments of the Northern Great Barrier Reef Province, Australia; Chapter 7. Infilling of Coastal Lagoons by Terrigenous Siliciclastic and Marine Carbonate Sediment: Vieques, Puerto Rico; Chapter 8. Carbonate Terrigenous Sedimentation on the North Puerto Rico Shelf; Chapter 9. Accumulation of Mixed Carbonate and Siliciclastic Muds on the Continental Shelf of Eastern Spain; Chapter 10. Carbonate to Siliciclastic Periplatform Sediments: Southwest Florida Chapter 11. Control of Terrigenous-Carbonate Facies Transitions by Baroclinic Coastal Currents Over the years, the field of sedimentology has become subdivided into various specialities. Two of the largest groups are those who study clastic rocks and those who study carbonates. There is little communication between the two: journals appear which are exclusively devoted to one or the other, and research conferences tend to be mutually exclusive. On the other hand, rocks themselves cannot be ""pigeon-holed"" in this way - the facies change from clastic to carbonate both laterally and through time. This volume stems from the editors' observations of such changes in the Gulf of Mexico a English Carbonate rocks Sedimentary rocks Electronic books Doyle, Larry J. Roberts, Harry H. 0-444-42904-2 Developments in sedimentology 42