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• W191750805 abstract "The energy sources that result in sediment particle associations, reorientation, and disaggregation are presented in terms of processes and mechanisms. Based on electron microscopy observations and theoretical considerations, the observed and modeled microfabric forms and signatures are associated with processes and mechanisms operating in various micro- and macroenvironments. The interplay of geological, chemical, and biological processes and mechanisms during transport, deposition, and burial of particulate material largely controls and ultimately determines the physical nature, properties, and observable micro- and macro-characteristics of soft sediments and their indurated equivalents. Discrete events such as suspended sediment transport, flocculation, and slumping may be identified and/or observed in the field or laboratory. More often, the sedimentary material is studied to understand and infer processes and mechanisms responsible for its fundamental properties, origin, significance, and stratigraphic position in the geological record. The particle-to-particle development and ultimate nature of a sedimentary deposit and its variability in time and space depend on multiple processes that include some important mechanisms that occur extremely fast and others that progress over eons." @default.
• W191750805 created "2016-06-24" @default.
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• W191750805 creator A5060182036 @default.
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• W191750805 date "1991-01-01" @default.
• W191750805 modified "2023-10-10" @default.
• W191750805 title "Determinants of Clay and Shale Microfabric Signatures: Processes and Mechanisms" @default.
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• W191750805 doi "https://doi.org/10.1007/978-1-4612-4428-8_2" @default.
• W191750805 hasPublicationYear "1991" @default.
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