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层序—岩相古地理演化及其对深层和超深层储层类型的控制:以四川盆地东北部二叠系茅口组为例

Sequence-lithofacies paleogeographic evolution and its control on deep and ultra-deep reservoir types: A case study of the Permian Maokou Formation in northeastern Sichuan Basin.

作者信息

Wang Xiandong, Tan Wancang, Lu Peng, Wang Ying, Li Qiang, Zhao Liang, Niu Pengfei, Cang Zhengyi, Gong Bao, Shen Jiagang

机构信息

The Exploration & Development Institute of Daqing Oil field Ltd.Company, Daqing, China.

College of Earth Science, Northeast Petroleum University, Daqing, China.

出版信息

PLoS One. 2025 Jul 1;20(7):e0327224. doi: 10.1371/journal.pone.0327224. eCollection 2025.

Abstract

The Middle Permian Maokou Formation in northeastern Sichuan Basin has been explored with continuous breakthroughs in recent years, but its sequence-lithofacies paleogeographic characteristics and tectonic-sedimentary evolution process are still unclear. Based on outcrops, well logging and seismic data, this paper focuses on the sequence stratigraphic, lithofacies paleogeography and tectonic-sedimentary evolution of the Maokou Formation in northeastern Sichuan Basin. The results show that two third-order sequences (SQ1, SQ2) are developed in the Middle Permian Maokou Formation. SQ1 can be divided into three fourth-order sequences (SQ1-1, SQ1-2, and SQ1-3). SQ1-1 and SQ1-2 are generally carbonate ramps, SQ1-3 turns to rimmed carbonate platform, and its stratigraphic thickness and sedimentary facies are distributed in NW-SE direction. The succession development of carbonate platform in SQ2 sedimentary period. It is believed that, due to the NE-trending extensional stress generated by the continuous subduction of the Mianlue Ocean and the regional sea level eustacy, the Permian tectonic-sedimentary differentiation in the northeastern Sichuan Basin had begun from the early stage of the Middle Permian and gradually intensified. As a result, the platform-basin dominated deep-water deposits gradually expanded into the basin along SW-NE direction, and evolved into the features of "platform in the south and platform-basin in the north" at the end of the Maokou Formation deposition. As such, large-scale high-energy shoals are developed above the platform region during the SQ1-3 and SQ2 depositional periods, making it a prospect of conventional gas. Potential source rocks are developed in the platform-basin region, which is a potential prospect of unconventional oil and gas. The results suggest that the tectonic-sedimentary differentiation induced by the continuous subduction of Mianlue Ocean makes the Maokou Formation an ideal reservoir for both conventional and unconventional hydrocarbon.

摘要

四川盆地东北部中二叠统茅口组近年来勘探不断取得突破,但其层序岩相古地理特征及构造沉积演化过程仍不清楚。本文基于露头、测井和地震资料,重点研究四川盆地东北部茅口组的层序地层、岩相古地理及构造沉积演化。研究结果表明,中二叠统茅口组发育两个三级层序(SQ1、SQ2)。SQ1可进一步划分为三个四级层序(SQ1-1、SQ1-2和SQ1-3)。SQ1-1和SQ1-2总体为碳酸盐缓坡,SQ1-3转变为镶边碳酸盐台地,其地层厚度和沉积相呈NW-SE向分布。SQ2沉积期碳酸盐台地继承性发育。研究认为,由于勉略洋持续俯冲产生的NE向拉张应力及区域海平面升降变化,四川盆地东北部二叠纪构造沉积分异从中二叠世早期开始并逐渐加剧。致使台盆相间的深水沉积沿SW-NE方向逐渐向盆地内部扩展,在茅口组沉积末期演变为“南台北盆”格局。因此,在SQ1-3和SQ2沉积期台地区发育大规模高能滩体,具备常规气勘探前景。台盆区发育潜在烃源岩,具备非常规油气勘探潜力。研究成果表明,勉略洋持续俯冲引起的构造沉积分异使茅口组成为常规和非常规油气的理想储层。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/4930/12212539/68aef731aa66/pone.0327224.g001.jpg

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