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Evaluation of Early Diagenesis in Modern, Shallow-Water Carbonate Sediments byMineralogy, Fabric and Porewater Geochemistry

机译：利用矿物学，织物和岩溶地球化学评价现代浅水碳酸盐岩沉积物早期成岩作用

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Mineralogy, fabric, and porewater geochemistry were examined in order to studyearly diagenesis in modern, shallow-water carbonate sediments of Key West area. The evidence for early diagenesis is visible as micritic cement in SEM images of sediment samples. Because the major cation concentrations are found to be insensitive to the diagenetic reactions in the study area, mineralogy instead of porewater geochemistry will be used to quantify the extent of early diagenesis. Rietveld crystal structure refinement method will be used for the accurate quantification of phase transformations. (MM).

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作者
Furukawa, Y.; Wiesenburg, D.;
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年度 1995
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总页数 10
原文格式 PDF
正文语种 eng
中图分类工业技术;
关键词
Sediments; Geochemistry; Carbonate minerals; Phase transformations; Physicalproperties; Shallow water; Pore pressure; Ph factor; Recrystallization; Benthonic zones; Carbonates;

机译：沉积物;地球化学;碳酸盐矿物;相变;物理性质;浅水;孔隙压力; ph因子;重结晶;底栖带;碳酸盐岩;

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Evaluation of Early Diagenesis in Modern, Shallow-Water Carbonate Sediments byMineralogy, Fabric and Porewater Geochemistry

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