吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (3): 645-658.doi: 10.13278/j.cnki.jjuese.20200141

• 地质与资源 •    下一篇

塔里木盆地顺北地区奥陶系油气充注过程分析

韩强1,2, 云露3, 蒋华山3, 邵小明2, 金仙梅2   

  1. 1. 西北大学地质学系, 西安 710069;
    2. 中国石化西北油田分公司勘探开发研究院, 乌鲁木齐 830011;
    3. 中国石化西北油田分公司, 乌鲁木齐 830011
  • 收稿日期:2020-06-20 发布日期:2021-06-07
  • 作者简介:韩强(1980—),男,博士研究生,高级工程师,主要从事石油地质研究,E-mail:105289562@qq.com
  • 基金资助:
    国家科技重大专项（2016ZX05005-004）；国家重点基础研究发展计划（"973"计划）项目（2016CB214806）

Marine Oil and Gas Filling and Accumulation Process in the North of Shuntuoguole Area in Northern Tarim Basin

Han Qiang1,2, Yun Lu3, Jiang Huashan3, Shao Xiaoming2, Jin Xianmei2   

  1. 1. Geology Department of Northwest University, Xi'an 710069, China;
    2. Institue of Exploration and Development of Northwest Branch, Sinopec, Urumqi 830011, China;
    3. Northwest Branch, Sinopec, Urumqi 830011, China
  • Received:2020-06-20 Published:2021-06-07
  • Supported by:
    Supported by the Major National Science and Technology Projects (2016ZX05005-004) and the National Key Basic Research and Development Program ("973" Program)(2016CB214806)

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摘要： 综合油气地球化学、流体包裹体和构造演化资料，对塔里木盆地顺北地区奥陶系不同断裂带油气性质差异性、成藏期次及油气充注过程进行研究。地球化学分析表明，顺北地区不同断裂带油气物性和成熟度存在差异，由西向东从7号断裂带向1号断裂带原油密度变小，西部的7号带和5号带北段油气成熟度低，5号带南段和1号带油气成熟度高。包裹体分析结果表明，顺北地区奥陶系油气藏存在加里东晚期、海西晚期及喜马拉雅期多期油气充注过程。自西向东不同断裂带上主成藏期存在差异，西部的7号及5号断裂带油气成藏期为加里东晚期和海西晚期，东部的顺北1号断裂带多了一个晚期油气成藏即喜马拉雅期成藏。顺北地区多期油气充注成藏是导致该区油气成熟度变化的主要原因。研究区奥陶系成藏期古构造对断裂带的油气充注具有控制作用。加里东晚期，研究区走滑断裂带构造均处于充注有利区；海西晚期，顺北11号断裂带及其以西地区充注来自东部满加尔的油气概率较低。喜马拉雅期，仅顺北1号断裂带及其以东获得高熟油气充注。

关键词: 海相油气, 流体包裹体, 油气运聚, 构造演化, 奥陶系, 顺北地区, 塔里木盆地

Abstract: The filling history and accumulation process of oil and gas reservoirs were studied by using the data of oil and gas geochemistry, fluid inclusions,and tectonic evolution. There are three periods of hydrocarbon accumulation in the Shuntuoguole area of the Tarim basin, which were in the Late Caledonian, Late Hercynian, and Himalayan. There are differences in the main reservoir forming periods between the different fault zones. The main hydrocarbon accumulation period in No.7 and No.5 fault zones in the west was in the Late Hercynian. In the Eastern Shunbei No.1 fault zone, not only the Late Hercynian hydrocarbon accumulation, but also Himalayan hydrocarbon filling occurred. The reasons for the change of physical properties of oil and gas are multi-stage oil and gas filling and Ordovician paleotectonic evolution. The oil and gas filling periods of the fault zone are controlled by the paleostructure. In the Late Caledonian period, the strike slip fault zone of the study area was located in the favorable area for charging of the oil and gas generated by the source rocks of Manjar depression in the eastern basin; in the Late Hercynian period, the charging opportunity with oil & gas from the Manjiaer depression in the west of the fault No.11 was low; In the Himalayan period, only the Shunbei fault No. 1 structural belt and its east obtained high-mature oil and gas filling.

Key words: marine oil and gas, fluid inclusions, hydrocarbon migration and accumulation, structural evolution, Ordovician, north Shuntuoguole area, Tarim basin

中图分类号: 

  • P618.13
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