Organic―inorganic interactions in petroleum-producing sedimentary basins

Jeffrey S. Seewald

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Organic―inorganic interactions in petroleum-producing sedimentary basins

机译：产油沉积盆地中的有机-无机相互作用

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Petroleum deposits form as a consequence of the increased temperatures that accompany progressive burial of organic matter deep within sedimentary basins. Recent advances in petroleum geochemistry suggest that inorganic sedimentary components participate in organic transformations associated with this process. Water is particularly important because it facilitates reaction mechanisms not available in dry environments, and may contribute hydrogen and oxygen for the formation of hydrocarbons and oxygenated alteration products. These findings suggest that petroleum generation and stability is influenced by subsurface chemical environments, and is a simple function of time, temperature and the composition of sedimentary organic matter.

机译：温度升高伴随沉积盆地深处有机物的逐渐埋葬而形成石油沉积。石油地球化学的最新进展表明，无机沉积组分参与了与此过程相关的有机转化。水之所以特别重要，是因为它促进了干燥环境中没有的反应机理，并且可能贡献氢和氧来形成碳氢化合物和氧化变化产物。这些发现表明，石油的产生和稳定性受地下化学环境的影响，并且是时间，温度和沉积有机物组成的简单函数。

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来源
《Nature》 |2003年第6964期|p.327-333|共7页
作者
Jeffrey S. Seewald;
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作者单位

Department of Marine Chemistry and Geochemistry, MS #4, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA;

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收录信息美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
原文格式 PDF
正文语种 eng
中图分类自然科学总论;
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Organic―inorganic interactions in petroleum-producing sedimentary basins

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