diagenetic deposit oor Spaans
diagenetic deposit
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depósito diagenético
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These variations reflect the original depositional process and subsequent diagenetic and tectonic changes.
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Smooth surfaces often denote slow, hydrogenetic (precipitation directly from seawater) metal accumulation in relatively low abundance, low grade deposits, while botryoidal surfaces and discoid nodule shapes indicate diagenetic (within the sediments) growth in relatively high grade, high abundance nodules.
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We have learned that this variability is due to the extreme complexity and variation with time of processes responsible for the formation of the earth's crust, from plate tectonics to erosion, sediment transport, and deposition, as well as to mechanical, climatic, and diagenetic effects.
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Cementation is the diagenetic process by which coarse clastic sediments become lithified or consolidated into hard, compact rocks, usually through the deposition or precipitation of minerals in the spaces between the individual grains of sediment.
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These results allows us to interpret precisely the lithostratigraphy of the deposits and the sedimentary and diagenetic processes responsible for their formation and evolution.
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Some features of this site may not work without it. Heavy-mineral analysis allows constraining provenance of detrital materials as well as their diagenetic history and the energetic characteristics o depositional environment.
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[ABSTRACT] The distal aluvial fan and the palustrine deposits of the Paracuellos de Jarama area display a variety of specific pedogenic and diagenetic features.
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Such results are necessary (1) to precisely reconstruct the conditions for hydrocarbon migration, (2) to determine the responsible mechanisms for porosity changes in a certain rock type and for the filling of reservoirs, (3) to understand the hydrodynamics ofpaleofluids in basins with associate formation of stratabound deposits, and (4) to better understand diagenetic processes.
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Conventionally and on very cursory inspection the deformations may be attributed to diagenetic processes by compression and compaction or to synsedimentary processes by the dynamics of the material’s deposition.
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ambiente freático somero o incluso vadoso. [ABSTRACT] The distal aluvial fan and the palustrine deposits of the Paracuellos de Jarama area display a variety of specific pedogenic and diagenetic features.
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This basin is a good example of cyclicity of different depositional sequences (DSs) in sedimentary environments, which show clear repetition in their sandstone composition (petrofacies) and diagenetic patterns.
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Cementation is the diagenetic process by which coarse clastic sediments become lithified or consolidated into hard, compact rocks, usually through the deposition or precipitation of minerals in the spaces between the individual grains of sediment.
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Cementation[edit] Cementation is the diagenetic process by which coarse clastic sediments become lithified or consolidated into hard, compact rocks, usually through the deposition or precipitation of minerals in the spaces between the individual grains of sediment.
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