鄂尔多斯盆地大牛地气田奥陶系马家沟组 原油裂解气形成及演化

作    者:姜海健1,2,蒋 宏1,2,张 威3,李春堂3,王 杰1,2,朱建辉1,2,王 萍1,2,张 毅1,2 朱茂1. 2,谭万仓3,和源5,朱可丹1, 2,徐哲航1, 2,朱心健1, 2,熊绍云1, 2,张豪1, 2
单    位:中国石化石油勘探开发研究院无锡石油地质研究所;2 中国石化油气成藏重点实验室; 3 中国石化华北油气分公司勘探开发研究院
基金项目:
摘    要:
近年来在鄂尔多斯盆地奥陶系马家沟组内幕(盐间及盐下段)取得了天然气勘探突破,深入研究天然气形成 及演化过程对内幕天然气勘探具有重要意义。以大牛地马家沟组气田为研究对象,通过对内幕岩心、薄片中沥青的 识别,烃类包裹体的产状及拉曼光谱测试,以及天然气地球化学指标分析,确定马家沟组天然气成因;综合油裂解气 的形成条件以及区域埋藏史和热史模拟结果,分析马家沟组内幕油气形成和演化过程。研究表明:大牛地气田马家 沟组缝洞储层中见沥青充填,方解石脉中也捕获了油、气和沥青三相烃类包裹体,均证实了存在油裂解气过程。马家 沟组内幕天然气以油裂解气为主,主要来源于马三段沉积期膏盐洼海相烃源岩;早侏罗世烃源岩大量生油,早白垩世 油裂解生成气,而且油气发生了TSR反应。受区域埋藏史和热史控制,研究区马家沟组烃源岩具有南部成熟早、北部 成熟晚的特征,天然气具有沿区域走滑断裂由南向北运聚的趋势。
关键词:碳酸盐岩;油型气;油裂解气;成藏模式;马家沟组;鄂尔多斯盆地

The formation and evolution of oil-cracked gas of the Ordovician Majiagou Formation in Daniudi gas field, Ordos Basin

Author's Name: JIANG Haijian1,2, JIANG Hong1,2, ZHANG Wei3, LI Chuntang3, WANG Jie1,2, ZHU Jianhui1,2, WANG Ping1,2, ZHANG Yi1,2
Institution: 1. Wuxi Institute of Petroleum Geology, SINOPEC Research Institute of Petroleum Exploration and Production; 2. SINOPEC Key Laboratory of Hydrocarbon Accumulation;
Abstract:
In recent years, natural gas exploration breakthrough has been made in the Ordovician Majiagou Formation of Ordos Basin, but the formation and evolution of natural gas have not been thoroughly studied. Taking Daniudi gas field as an example, the typical characteristics of oil-cracked gas in Majiagou Formation are determined through the identification of bitumen in the core and thin section, the occurrence of hydrocarbon inclusions and Raman spectroscopy testing, and the analysis of geochemical data of natural gas. The formation conditions of oil-cracked gas are comprehensively analyzed, and the formation and evolution process of oil-cracked gas in Majiagou Formation are analyzed through the simulation of burial history and thermal history. The results show that: (1) Bitumen filling with diverse occurrences is found in the fractured porous reservoir of Majiagou Formation, and it is a dry bitumen with high degree of thermal evolution. Three phase hydrocarbon inclusions of oil, gas and bitumen are captured in calcite veins of Majiagou Formation, which confirms the existence of oil cracking gas process. (2) Based on the crossplot of geochemical index such as ln(C1/C2) and ln(C2/C3) of natural gas, it shows that the internal natural gas of Majiagou Formation is mainly oil-cracked gas. (3) During the deposition period of 3rd member of Majiagou Formation, Daniudi and its surrounding areas were situated at the margin of a saline depression, where thick source rocks of argillaceous dolomite and dolomitic mudstone developed with interbedded evaporates, creating favorable conditions for thermochemical sulfate reduction (TSR). (4) In the Early Jurassic, source rocks produced a large amount of oil. Under the effect of the relatively high paleotemperature in the Early Cretaceous, high-temperature oil cracking occurred, and TSR reaction occurred with significantly increased H2S content in the natural gas of O1m55 -O1m56 of Majiagou Formation in Daniudi gas field. (5) In Daniudi and surrounding areas, the source rocks of Majiagou Formation became mature earlier in the south and later in the north, and natural gas mainly migrated and accumulated from south to north along the strike-slip faults. This study has certain significance for the internal gas exploration of Majiagou Formation in Ordos Basin.
Keywords: carbonate rock; oil type gas; oil cracked gas; hydrocarbon accumulation; Majiagou Formation; Ordos Basin
投稿时间: 2025-06-30  
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