Titlebook: Carbonate Microfabrics; Richard Rezak (Professor Emeritus),Dawn L. Lavoie Book 1993 Springer-Verlag New York, Inc. 1993 chemistry.fabric.g

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Mathematical Analysis of Fluids in Motioneration of ooids. Channels are oriented perpendicular to the axis of highest ooid concentration and are linked to the transport system by their ebb-tidal deltas..On Joulters Cays, Bahamas, surface samples and cores from four channels provide information on trends of microfabrics that should be usefu

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Paolo Antonelli,Pierangelo Marcati texture and fabric. This is possible because, during the past two decades, the carbonate mudbanks of south Florida have been re-examined through a series of detailed stratigraphic studies (Wanless, 1976 and 1979; Warzeski, 1976; Enos and Perkins, 1979; Cottrell, 1989; Tagett, 1989; Wanless and Tage

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https://doi.org/10.1007/978-1-4419-9554-4structure and descends to a base level of accumulation in hollows and on ledges. In the inner recesses sediment settles out of suspension, and where it only partially fills cavities, geopetal fabrics are created. Once deep inside the structure the internal sediment is usually trapped in its final re

acrimony

https://doi.org/10.1007/3-540-29264-0f fine-grained magnesian calcite. Most cementation occurs at slope depths within the permanent thermocline (200 to 800 m) and in areas of well-developed, long-slope currents..The overall effect of this process is to create muddy (micritic) lithologic units from originally mud-free sediments, thereby

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Computational Fluid and Solid Mechanicsacts on Louisiana’s continental slope has led to the realization that authigenic carbonates are extremely abundant in locations where hydrocarbon seeps occur. These carbonates range from nodules formed in near-surface sediments, to massive reef-like buildups of yet unknown age that commonly have 20

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Eduardo N. Dvorkin,Marcela B. Goldschmitogists are recognizing the possibility that bacterially induced precipitates may form significant mineral deposits. Unfortunately, there are currently no criteria by which they can be recognized in Recent sediments, or in the rock record..Cultures of aerobic and facultative bacteria from cyanobacter

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https://doi.org/10.1007/3-540-29264-0verburden pressure. Most marine clays consist of smectites and illites that are fine-grained and platey. In contrast, carbonate sediments are composed of multishaped, multisized components. In general, clay-rich sediments consolidate to lower porosities and are less permeable than carbonates at give

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