About: Sedimentary structures is a research topic. Over the lifetime, 2882 publications have been published within this topic receiving 77507 citations.
TL;DR: In this article, a model of transverse bedforms in Unidirectional Flows is presented, along with cross-stratification patterns of Ripples and Dunes in Changing Flows.
Abstract: 1. Environmental Fluid Dynamics. 2. Entrainment and Transport of Sedimentary Particles. 3. Particle Motions at Low Concentrations: Grading in Pyroclastic-Fall Deposits. 4. Packing of Sedimentary Particles. 5. Orientation of Particles During Sedimentation: Shape-Fabrics. 6. Transition to Turbulence and the Fine Structure of Steady Turbulent Boundary Layers: Parting Lineation and Related Structures. 7. Models of Transverse Bedforms in Unidirectional Flows. 8. Empirical Character of Ripples and Dunes Formed By Unidirectional Flows. 9. Climbing Ripples and Dunes and Their Cross-Stratification Patterns. 10. Bedforms in Supercritical and Related Flows: Transverse Ribs, Rhomboid Features, and Antidunes. 11. Transverse Bedforms in Multidirectional Flows: Wave-Related Ripples Marks, Sand Waves, and Equant Dunes. 12. Ripples and Dunes in Changing Flows.
TL;DR: For more than 100 years geologists have been ex amining and describing modern sediments with an eye toward using characteristic features to aid in the interpretation of depositional settings of ancient strata.
Abstract: For more than 100 years geologists have been ex amining and describing modern sediments with an eye toward using characteristic features to aid in the interpretation of depositional settings of ancient strata. This field of interest developed particularly during the 1950s and 1960s with the creation of detailed models for modern carbonate deposition in Florida, the Bahamas, Cuba, the Persian Gulf, Belize, Pacific atolls, the Great Barrier Reef and other areas. An understanding of the depositional environments of these modern models, coupled with increased understanding of diagenetic effects, has led to vastly improved interpretations of ancient limestones. Such models also improved the “predictability” of many carbonate reservoir rocks.
In spite of the great strides made in our knowledge about carbonate depositional environments, their characteristic features have never been synthesized in a single work. Although excellent textbooks exist which describe some aspects of the interpretation of both ancient strata and modern sediments, systematic treatment of the entire subject is available only in the primary literature.
This book is an attempt to bring together this widely disseminated literature. The volume is specifically designed for use by the non—specialist-the petroleum geologist or field geologist—who needs to use carbonate depositional environments in facies reconstructions and environmental interpretations. Yet it is hoped that the book will also serve as a valuable reference for the specialist or advanced graduate student.
Toward that purpose, the book is extensively illustrated with color diagrams and photographs of sedimentary structures and facies assemblages. The text focuses on the recognition of depositional environments rather than on the hydrodynamic mechanisms of sediment movement.
TL;DR: In this article, the authors discuss the transport and deposition of Siliciclastic Sediment and its relationship with other Chemical/Biochemical and Carbonaceous Sedimentary Rocks, as well as their relationship with geologic time.
Abstract: 1. Weathering and Soils 2. Transport and Deposition of Siliciclastic Sediment 3. Sedimentary Textures 4. Sedimentary Structures 5. Siliciclastic Sedimentary Rocks 6. Carbonate Sedimentary Rocks 7. Other Chemical/Biochemical and Carbonaceous Sedimentary Rocks 8. Continental (Terrestrial) Environments 9. Marginal-Marine Environments 10. Siliciclastic Marine Environments 11. Carbonate and Evaporite Environments 12. Lithostratigraphy 13. Seismic, Sequence, and Magnetic Stratigraphy 14. Biostratigraphy 15. Chronostratigraphy and Geologic Time 16. Basin Analysis, Tectonics, and Sedimentation