南黄海与上扬子地区中、古生代海相岩石地层对比

Guo Xing-wei
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引用次数: 13

摘要

近年来,海相油气勘探受到了中国的高度重视。南黄海广泛分布前新生代海相地层。为了更好地了解这些地层,本文利用南黄海的钻井资料和上扬子地区的岩石地层资料,对南黄海与四川盆地上扬子海相地层及其沉积特征进行了对比。结果表明,以碳酸盐岩台地沉积为主的两区中、古生代海相地层在印支期运动前大体相似,但受古生代和中生代构造运动的影响,在时间和规模上存在差异。长江上游和下游的沉积物具有可比性。并简要讨论了两区烃源岩和储层的储集能力。四川盆地海相油气勘探的成功为南黄海海相油气潜力评价和油气勘探提供了参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
LITHOSTRATIGRAPHIC CORRELATION OF MESOZOIC AND PALAEOZOIC MARINE STRATA BETWEEN SOUTH YELLOW SEA AND UPPER YANGTZE REGION
Exploration for marine hydrocarbon has gained great attention in China recently.The Pre-Cenozoic marine strata were widely distributed in the South Yellow Sea.In order to better understand these strata,we made comparison in this article of the marine strata and their depositional features between the South Yellow sea and the Sichuan basin in the upper Yangtze with the well data from the South Yellow sea and the lithostratigraphic data from the Upper Yangtze area.It is concluded that the Mesozoic and Paleozoic marine strata in the two areas dominated by carbonate platform deposits are generally similar before Indosinian movement,but different in the time and scale due to the tectonic movements in Paleozoic and Mesozoic.The sediments are comparable between the upper and lower Yangtze.Also discussed briefly are the source rocks and reservoir storage capabilities between the two regions.The successful exploration for marine oil and gas in the Sichuan Basin has provided a benchmark for the assessment of oil and gas potential and exploration of marine hydrocarbons in the South Yellow Sea.
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