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准噶尔盆地石炭系烃源岩发育特征及分布规律

吴孔友 李冰冰 宋志华 程贝涛 曹立刚 王金友

浙江大学学报(理学版)2026,Vol.53Issue(4):521-534,14.
浙江大学学报(理学版)2026,Vol.53Issue(4):521-534,14.DOI:10.3785/1008-9497.25074

准噶尔盆地石炭系烃源岩发育特征及分布规律

Development characteristics and distribution patterns of Carboniferous source rocks in the Junggar Basin

吴孔友 1李冰冰 1宋志华 2程贝涛 1曹立刚 3王金友1

作者信息

  • 1. 中国石油大学(华东) 地球科学与技术学院,山东 青岛 266580
  • 2. 中国石油新疆油田公司勘探事业部,新疆 克拉玛依 834000
  • 3. 中国石油集团东方地球物理勘探有限责任公司,河北 涿州 072751
  • 折叠

摘要

Abstract

As oil and gas exploration in China progressively extends to deeper layers,the Carboniferous in the Junggar Basin has become a key exploration target.It has been not only found to contain abundant oil and gas resources but also confirmed as a high-quality source rock.Based on the drilling,seismic and outcrop data,combined with gravity,magnetic,and electrical data,this study investigates the development characteristics and laws of distribution of Carboniferous source rocks in the Junggar Basin,defines the hydrocarbon generation centers,and reveals the main control factors of source rock development based on the analysis of the evolution process of sedimentary paleogeographic environment,in order to deepen the understanding of the source rocks in the basin.The results of the study show that:(1)Three sets of main source rocks are developed in the Carboniferous of the Junggar Basin,including the Dishuiquan Formation(C1d)of the Lower Carboniferous,the b member of the Songkaersu Formation(C1sb)and the Shiqiantan Formation(C2sh)of the Upper Carboniferous.Its lithology is mainly composed of mudstone and tuffaceous mudstone,followed by carbonaceous mudstone,The main type of organic matter in source rocks is type Ⅲ,which is basically in a highly mature evolutionary stage,mainly producing gas.(2)The development of C1d and C2sh source rocks is mainly controlled by the sedimentary environment of marine and continental transitional facies,while the C1sb source rocks are formed during the intermittent period of volcanic eruptions,and the tuff provides favorable conditions for the development of source rocks.(3)Seven hydrocarbon source kitchens are formed in the whole basin,which are mainly distributed in the eastern sag area of the basin.The degree of confirmation of the C1d source rock is lower than that of the source rocks in C1d,C1sb and C2sh.

关键词

准噶尔盆地/石炭系/烃源岩/发育特征/沉积环境/分布规律

Key words

Junggar Basin/Carboniferous/source rock/developmental characteristics/sedimentary environment/distribution pattern

分类

能源科技

引用本文复制引用

吴孔友,李冰冰,宋志华,程贝涛,曹立刚,王金友..准噶尔盆地石炭系烃源岩发育特征及分布规律[J].浙江大学学报(理学版),2026,53(4):521-534,14.

基金项目

国家自然科学基金面上项目(42272155) (42272155)

新疆维吾尔自治区重大科技专项(2024A01010). (2024A01010)

浙江大学学报(理学版)

1008-9497

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