Characteristics and hydrocarbon significances of paleo-bay in fourth member of Middle Triassic Leikoupo Formation, western Sichuan Basin, SW China

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  • 1. State Key Laboratory of Oil & Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China;
    2. Xihua University, Chengdu 610039, China;
    3. PetroChina Tarim Oilfield Company, Korla 841000, China;
    4. PetroChina Research Institute of Petroleum Exploration and Development, Beijing 100083, China

Received date: 2024-03-29

  Revised date: 2024-10-10

  Online published: 2024-10-31

Abstract

The depositional facies types of the fourth member of the Middle Triassic Leokoupo Formation (Lei-4 Member) in western Sichuan Basin are examined through the methods of sedimentology, lithology and the mineral composition interpretation, as well as the special lithofacies indicators such as microbialite, anhydrite-halite succession and tempestites, using the data of about 400 boreholes and 11 outcrop sections. The distribution evolution characteristics and its hydrocarbon significances of the paleo-bay facies have been discussed further. The Lei-4 Member in western Sichuan Basin has an ocean-bay-flat depositional model, with the presence of evaporated tidal flat, restricted tidal flat and paleo-bay facies from east to west. The subfacies such as bay margin, subtidal bay and bay slope are recognized within the paleo-bay, with microbial reef and grain bank microfacies in the bay margin, microbial dolomitic flat, deep-water spongy reef and hydrostatic mudstone microfacies in the subtidal bay, and tempestites and collapsed deposits in the upper bay slope. The bay margin covered the Guangyuan-Zitong-Dujiangyan area in the period of the first submember of the Lei-4 Member (Lei-4-1), regressed westward into the Shangsi-Jiangyou-Dujiangyan area in the period of Lei-4-2, and expanded to the Jiange-Zitong-Langzhong-Wusheng-Yanting-Chengdu area in the northern part of central Sichuan Basin in the period of Lei-4-3 along with a small-scale transgression. The topographic pattern of “one high and two lows” is confirmed in the Lei-4 Member, corresponding to a configuration of source rocks and reservoir rocks that are alternated horizontally and superimposed vertically. Two efficient source-reservoir configuration models, i.e. side source & side reservoir, and self-generating & self-storing, are available with the microbial reef and grain bank reservoirs at the bay margin and the high-quality source rocks within the sags on both sides of the bay. The research findings will inevitably open up a new situation for the hydrocarbon exploration in the Leikoupo Formation.

Cite this article

SONG Jinmin, LIU Shugen, LI Zhiwu, XIA Shun, FENG Yuxiang, YANG Di, YE Yuehao, SHAO Xingpeng, WANG Bin, WANG Jiarui, JIN Xin, REN Shan, YANG Shaohai, LUO Ping . Characteristics and hydrocarbon significances of paleo-bay in fourth member of Middle Triassic Leikoupo Formation, western Sichuan Basin, SW China[J]. Petroleum Exploration and Development, 0 : 20241202 -20241202 . DOI: 10.11698/PED.20240202

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