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The Distribution Characteristics and Geological Significance of Inclusion Trace Elements in Silurian Oil-containing Sandstones in the Central Tarim Basin

机译:塔里木盆地中部志留系含油砂岩中包裹体微量元素的分布特征及地质意义

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摘要

Trace elements of fluid inclusion in 16 Silurian oil-containing sandstones from 10 wells in Tazhong area were performed by inductively coupled plasma mass spectroscopy (ICP-MS), the distribution characteristics were analyzed, and their demonstrative geological significance was deeply discussed. The results show that the abundance of trace element varied markedly in the same well field or different well fields, the distribution rule of the main trace elements is that the abundance is increasing as a whole from down structure location to structural high. Variation characteristics of single trace element are consistent with the trace element suite, which reflects Silurian hydrocarbons in Tazhong area migrated toward structural high or stratigraphic pinch-out direction, from northwest to southeast on the plane. Therefore, trace elements of fluid inclusion can provide effective evidence for studying oil and gas migratory direction.
机译:利用电感耦合等离子体质谱法(ICP-MS)对塔中地区10口志留系含油砂岩中的流体包裹体进行了微量元素分析,分析了其分布特征,并深入探讨了它们的地质意义。结果表明,同一井场或不同井场中微量元素的丰度变化显着,主要微量元素的分布规律是从下构造位置到上构造高点,总体上丰度增加。单一微量元素的变化特征与微量元素组相一致,反映了塔中地区志留系碳氢化合物从平面上向西北向东南向构造性高或地层扩展方向迁移。因此,流体包裹体中的微量元素可以为研究油气的迁移方向提供有效的证据。

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