Geochemical transformations of sedimentary sulfur.
Geochemical transformations of sedimentary sulfur.
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DOI：
10.1021/bk-1995-0612
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发表时间：
1995-05
期刊：
影响因子：
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通讯作者：
M. Vairavamurthy;M. Schoonen;T. Eglinton;G. Luther;B. Manowitz
中科院分区：
文献类型：
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作者：
M. Vairavamurthy;M. Schoonen;T. Eglinton;G. Luther;B. Manowitz
硫在沉积体系中的化学转化研究是地球化学的前沿研究领域，对这一领域的深入了解对许多地球化学学科都至关重要。目前硫地球化学的研究是多种多样的，跨越主题的低温转化在早期成岩作用的热反应在后期成岩作用的退化。它包括有机、无机和生物化学方面。本卷基于1994年美国化学学会专题讨论会，提供了与沉积硫转化有关的复杂地球化学过程的最新研究的跨学科观点。这一主要章节概述了沉积硫转化的主要地球化学途径，强调海洋系统。
The study of chemical transformations of sulfur in sedimentary systems is a frontier research area in geochemistry, and a fuller knowledge of this field is crucial to many geochemical disciplines. Current research on sulfur geochemistry is diverse, spanning topics in low temperature transformations in early diagenesis to the thermal reactions during later diagenesis to catagenesis. It embraces organic, inorganic and biochemical aspects. The present volume provides an interdisciplinary view of recent research on the complex geochemical processes related to sedimentary sulfur transformations based on the 1994 American Chemical Society Symposium. This leading chapter gives an overview of the major geochemical pathways of sedimentary sulfur transformations, emphasizing marine systems.