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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书目名称Carbonate Microfabrics影响因子(影响力)




书目名称Carbonate Microfabrics影响因子(影响力)学科排名




书目名称Carbonate Microfabrics网络公开度




书目名称Carbonate Microfabrics网络公开度学科排名




书目名称Carbonate Microfabrics被引频次




书目名称Carbonate Microfabrics被引频次学科排名




书目名称Carbonate Microfabrics年度引用




书目名称Carbonate Microfabrics年度引用学科排名




书目名称Carbonate Microfabrics读者反馈




书目名称Carbonate Microfabrics读者反馈学科排名

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Carbonate Microfabrics Related to Subaerial Exposure and Paleosol Formationle, dune and beach sands display pronounced development of subaerial microfabric features. Pleistocene grainstones from San Salvador, Bahamas, contain rhizoliths, pedotubules, alveolar textures, calcified root hairs, Microcodium, laminated micrite, clotted micrite, soil pisoids, circumgranular crack

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cumber

Depositional and Early Diagenetic Controls on Texture and Fabric of Carbonate Mudbanks, South Florid 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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泥瓦匠

泥瓦匠

Cold-Seep Carbonates of the Louisiana Continental Slope-to-Basin Flooracts 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

Nausea

Habit of Bacterially Induced Precipitates of Calcium Carbonate: Examples from Laboratory Experimentsogists 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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Permeability Characteristics of Continental Slope and Deep-Water Carbonates from a Microfabric Perspverburden 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

foreign

Microfabric and Physical Properties of Deep-Sea High Latitude Carbonate Oozesiceous ooze facies. These biogenous oozes are accumulations of the skeletons and skeletal fragments of calcareous and biosiliceous phytoplankton and zooplankton (nannofossils and foraminifers versus diatoms and radiolaria, respectively), which once lived in the upper water column. This “rain” of mic