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OALib Journal期刊
ISSN: 2333-9721
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鄂尔多斯盆地西南部与中东部奥陶系马家沟组碳酸盐岩地球化学特征对比
Keywords: 鄂尔多斯盆地,马家沟组,有机碳,饱和烃,生物标志化合物
Abstract:
？鄂尔多斯盆地奥陶系马家沟组碳酸盐岩是否能够作为有效烃源岩以及有效烃源岩的主要分布区域，这对中部气田天然气来源的认识至关重要。通过对比研究鄂尔多斯盆地西部、南部和中东部地区奥陶系马家沟组碳酸盐岩有机碳含量、氯仿沥青”a”含量以及饱和烃生物标志化合物特征，分析其与鄂尔多斯盆地马家沟组沉积环境的关系，认为鄂尔多斯盆地西部和南部以开阔海相沉积为主的马家沟组碳酸盐岩沉积于弱氧化—弱还原环境，有机碳含量普遍低，toc值高于0.3%的有效气源岩所占比例低；中东部以咸化潟湖或台地蒸发沉积为主的奥陶系马家沟组碳酸盐岩沉积于强还原环境，有机碳含量高于西部和南部马家沟组碳酸盐岩，toc值高于0.3%的有效气源岩所占比例较高，很有可能是中部气田奥陶系来源天然气，即油型气的主要烃源岩。
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