Geology of Mudstones Atop the Sangonghe Formation, Shuixigou Group, Turpan-Hami Basin: New Insights and Their Implications for Petroleum Geology

IF 1.4 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Geological Journal Pub Date : 2024-11-13 DOI:10.1002/gj.5094
Weiming Wang, Meishuo Hu, Xuan Chen, Qingguo Liu, Weihao La, Hua Zhang, Yuzhong Yang, Changsheng Miao, Tingting Li
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Abstract

As the exploration of deep-seated oil and gas resources in the Turpan-Hami Basin intensifies, there is an urgent need to thoroughly depict the geological characteristics of newly uncovered, underexplored strata in sub-sag centers. This study undertakes the inaugural systematic geochemical analysis of mudstones atop the Sangonghe Formation, including palynological identification, maceral identification, biomarker analysis, total organic carbon (TOC) analysis, and pyrolysis. The findings reveal that the mudstone sequence, as the target layer, was deposited in a warm and moist paleoclimate and a weakly reducing to weakly oxidising saline water environment, fostering the growth of prolific algae and bacteria, thus ensuring substantial foundational materials for source rock formation. The organic matter in the mudstone sequence displays pronounced laminar accumulation. Despite the overall modest abundance, the organic matter features notable hydrocarbon-generating potential per unit of organic carbon and favourable types. Humic-sapropelic kerogens (type II1) are found in the mudstones, with organic matter generally reaching a mature to highly mature stage. These characteristics establish the mudstones as effective source rocks, furthermore, the hydrocarbon expulsion in the Xishanyao Formation precedes that of the Sangonghe Formation and that both formations constitute a sequential process in terms of hydrocarbon generation and expulsion timing and hydrocarbon contribution. Reanalyzing this mudstone sequence not only revises prior geological understanding of it as direct cap rocks, but also facilitates the reclassification of deep-seated strata into three distinct petroleum systems. Centered around this source rock layer, dual modes, namely the “lower-source rock and upper-reservoir” and the “ lower-reservoir and upper-source rock” modes can be formed. These new insights will offer profound implications for hydrocarbon resource evaluation and future hydrocarbon exploration endeavours in the Shuixigou Group within the Taibei sag.

吐哈盆地水西沟群三工河组泥岩地质新认识及其油气地质意义
随着吐哈盆地深层油气资源勘探力度的加大,迫切需要对凹陷中心新发现、未勘探地层的地质特征进行全面描述。本研究首次对三工河组泥岩进行了系统的地球化学分析,包括孢粉学鉴定、显微组分鉴定、生物标志物分析、总有机碳(TOC)分析和热解分析。研究结果表明,泥岩层序作为目标层,沉积于温暖湿润的古气候和弱还原-弱氧化咸水环境,促进了藻类和细菌的大量生长,为烃源岩的形成提供了大量的基础物质。泥岩层序中有机质呈明显的层状聚集。尽管有机质总体丰度不高,但单位有机碳生烃潜力显著,类型有利。泥岩中存在腐殖—腐泥型干酪根,有机质普遍处于成熟至高成熟阶段。这些特征表明,泥岩是有效烃源岩,西山窑组排烃先于三工河组排烃,两组在生排烃时间和油气贡献上是一个连续的过程。对该泥岩层序的重新分析,不仅修正了前人对其作为直接盖层的认识,而且有助于将深层地层重新划分为三个不同的含油气系统。以该烃源层为中心,可形成“下源上储”和“下储上源”双重模式。这些新发现将对台北凹陷水西沟组油气资源评价和油气勘探具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geological Journal
Geological Journal 地学-地球科学综合
CiteScore
4.20
自引率
11.10%
发文量
269
审稿时长
3 months
期刊介绍: In recent years there has been a growth of specialist journals within geological sciences. Nevertheless, there is an important role for a journal of an interdisciplinary kind. Traditionally, GEOLOGICAL JOURNAL has been such a journal and continues in its aim of promoting interest in all branches of the Geological Sciences, through publication of original research papers and review articles. The journal publishes Special Issues with a common theme or regional coverage e.g. Chinese Dinosaurs; Tectonics of the Eastern Mediterranean, Triassic basins of the Central and North Atlantic Borderlands). These are extensively cited. The Journal has a particular interest in publishing papers on regional case studies from any global locality which have conclusions of general interest. Such papers may emphasize aspects across the full spectrum of geological sciences.
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