塔里木盆地满西地区寒武系台地边缘分段演化及勘探目标

IF 3.6
Zongquan Hu , Fan Feng , Chengming Fang , Zicheng Cao , Tieyi Wang , Kangkang Guo , Yang Li , Shi Wang
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引用次数: 0

摘要

塔里木盆地寒武系地台边缘具有良好的生储盖组合,是超深—超深相控地层油气勘探的重要目标。在中国西部三大盆地中,塔里木盆地是唯一一个尚未取得勘探突破的大型台缘盆地。通过精细层序地层划分和分段分析,确定了满西地区寒武纪满西地台边缘的垂向和侧向差异演化。根据不同古地貌的发育和地台的演化过程,地台边缘由北向南可划分为玉起段、塔河段、顺北段和古城段。玉起段和顺北段呈现相对低海拔的古地貌。在早寒武纪,这两个段都处于海底构造阶段,导致储层总体规模有限。古城段具有海拔最高的古地貌,因此住宿空间有限。因此,高能量相带的快速横向运移导致了厚度有限的大型储层的发育。塔河段古地貌海拔较高,是形成大型储层的最有利段。台地边缘盖层以海侵期形成的礁后白云质平原和致密碳酸盐岩为主。通过对烃源岩、储层和盖层的综合评价,认为塔河段在台地边缘具有最佳的油气成藏条件。其中,沙伊里克组海侵沉积和吴松格尔组台地边缘高能丘滩杂岩构成了最佳的储盖组合,是台地边缘油气勘探最有希望的目标段。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Segmented evolution and exploration targets of the Cambrian platform margin in the Manxi area, Tarim Basin

Segmented evolution and exploration targets of the Cambrian platform margin in the Manxi area, Tarim Basin
The Cambrian platform margin in the Tarim Basin boasts favorable source-reservoir-cap assemblages, making it a significant target for hydrocarbon exploration in ultra- to extra-deep facies-controlled formations. Of the three major basins in western China, Tarim is the only basin with large-scale platform margin where no exploration breakthrough has been achieved yet. This study determines the vertical and lateral differential evolution of the platform margin (in the Manxi area hereafter referred to as the Cambrian Manxi platform margin) through fine-scale sequence stratigraphic division and a segmented analysis. The platform margin can be divided into the Yuqi, Tahe, Shunbei, and Gucheng segments, from north to south, based on the development of different ancient landforms and the evolutionary process of the platform. The Yuqi and Shunbei segments exhibit relatively low-elevation ancient landforms. Both segments were in a submarine buildup stage during the Early Cambrian, resulting in overall limited scales of their reservoirs. The Gucheng segment features the highest-elevation ancient landforms and accordingly limited accommodation spaces. As a result, the rapid lateral migration of high-energy facies zones leads to the development of large-scale reservoirs with only limited thicknesses. In contrast, the Tahe segment, exhibiting comparatively high-elevation ancient landforms, is identified as the most favorable segment for the formation of large-scale reservoirs. The cap rocks of the platform margin are dominated by back-reef dolomitic flats and tight carbonate rocks formed in transgressive periods. A comprehensive evaluation of source rocks, reservoirs, and cap rocks indicates that the Tahe segment boasts the optimal hydrocarbon accumulation conditions along the platform margin. In this segment, the Shayilike Formation transgressive deposits and the high-energy mound-shoal complexes along the platform margin of the Wusonggeer Formation constitute the optimal reservoir - cap rock assemblage, establishing this segment as the most promising target for hydrocarbon exploration in the platform margin.
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