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The Caspian Sea Basin: Tectonic Events and Sedimentation at the Turn of the Early-Middle Carboniferrous and the Formation of Oil and Gas Reservoirs

机译:里海盆地:早期中部碳酸盐岩之交的构造事件和沉积以及油气储层的形成

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摘要

A structural-facies map of the Bashkir stage of the Caspian basin, the southeastern part of the East European platform and the Turan plate is compiled on the basis of drilling data generalization. The sequence of tectonic events and sedimentation processes in the early late Bashkir century of the middle Carboniferous was reconstructed. It is shown that cessation of reef formation, appearance of erosion surfaces and partial destruction of the side ledges of Caspian depression occurred under the influence of Varis orogenesis and the global fall of the World Ocean level due to the glaciation of the Paleogondvana at the turn of earlymiddle Carboniferous. It is assumed that oil and gas reservoirs in the rocks of ViseBashkir age are confined to large bodies of carbonate-clastic rocks with clinoform structure that arose on the slopes of the depression due to destruction of its side ledges.
机译:在钻井数据综合的基础上,编制了里海盆地巴什基尔期,东欧平台东南部和图兰板块的结构相图。重建了中石炭纪巴什基尔世纪晚期晚期的构造事件和沉积过程的顺序。研究表明,在瓦里斯造山作用和世界海洋水平面的全球性下降的影响下,由于古罗马纪瓦纳河的转弯,珊瑚礁的形成停止,侵蚀面的出现和里海depression陷侧缘的部分破坏发生了。早中石炭世。假定维谢巴什基尔时代的岩石中的油气储集层被限制在大的碳酸盐岩碎屑岩体中,这种碳酸盐岩碎屑岩由于凹陷的边壁被破坏而出现在凹陷的斜坡上。

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