伦坡拉盆地始新统牛堡组烃源岩成熟史

潘磊; 曹强; 刘一茗; 李一腾; 汪岩; 李智泉

doi:10.11781/sysydz201603382

伦坡拉盆地始新统牛堡组烃源岩成熟史

doi: 10.11781/sysydz201603382

潘磊¹,
曹强^2, ,,
刘一茗²,
李一腾²,
汪岩²,
李智泉²

1.
中国石化勘探分公司, 成都 610041
2. 中国地质大学(武汉) 资源学院, 武汉 430074

基金项目: 中国石化重大勘探导向项目"西藏中石化探区油气勘探潜力评价与勘探部署建议"和中国石化勘探分公司横向协作项目(G0800-14-KK-169)资助。

详细信息

作者简介:
潘磊(1984-),男,工程师,从事石油地质综合研究工作。E-mail:panl.ktnf@sinopec.com。

通讯作者:
曹强(1983-),男,博士,讲师,从事油气地化及成藏方面研究。E-mail:qcao@cug.edu.cn。

中图分类号: TE122.1
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出版历程
- 收稿日期: 2016-01-25
- 修回日期: 2016-04-05
- 刊出日期: 2016-05-28

Maturity history of source rocks in the Eocene Niubao Formation, Lunpola Basin

1.
SINOPEC Exploration Company, Chengdu, Sichuan 610041, China
2. Faculty of Resources, China University of Geosciences, Wuhan, Hubei 430074, China

摘要

摘要: 伦坡拉盆地自下而上发育始新统牛堡组牛二中亚段、牛二上亚段及牛三下亚段3套烃源岩。基于钻井测试资料、地震资料及含烃流体包裹体测试分析,利用盆地模拟技术对伦坡拉盆地热史及牛堡组3套烃源岩的成熟史进行了系统分析。研究表明,伦坡拉盆地自始新统牛三段沉积以来直至渐新统丁青湖组三段沉积末期,古地温梯度总体表现为持续降低,变化介于6.67~4℃/hm,为典型热盆特征,古地温梯度升高与区域构造隆升作用具有明显的相关性。牛二中及牛二上亚段的2套烃源岩成熟较早且热演化程度高,分别于中-晚始新世(距今约46.4~37.5 Ma)及早渐新世(距今约36.6~33.5 Ma)进入生油门限,现今主体皆位于成熟生油阶段(R_o=0.7%~1.3%),是该区主力烃源岩。西部蒋日阿错洼陷牛二中及牛二上亚段主力烃源岩现今热演化程度最高,生供烃条件较中-东部江加错、爬错洼陷更为优越。
- 热史 /
- 成熟史 /
- 烃源岩 /
- 牛堡组 /
- 始新统 /
- 伦坡拉盆地
Abstract: Three sets of source rocks developed upwards in the Eocene Niubao Formation in the Lunpola Basin, i.e., the middle part of the second member of Niubao Formation (E₂n₂²), the upper part of the second member of Niubao Formation (E₂n₂³), and the lower part of the third member of Niubao Formation (E₂n₃¹). Based on drilling, seismic and hydrocarbon fluid inclusion analyses, the thermal evolution history of the basin and the maturity history of source rocks in the Niubao Formation were systematically analyzed with basin simulation technology. From the E₂n₃ to the third member of the Oligocene Dingqinghu Formation, the paleogeothermal gradient in the Lunpola Basin consistently decreases from 66.7 to 40℃/km, showing the characteristics of a typical heating basin. The growth of paleogeothermal gradient is clearly related to regional tectonic uplifting. The source rocks in the E₂n₂² and E₂n₂³ became mature early and have a higher maturity. They entered oil generation thresholds during the middle-late Eocene (46.4-37.5 Ma) and early Oligocene (36.6-33.5 Ma), respectively. At present, they are mature and generating oil (R_o=0.7%-1.3%), and serve as the main source rock in the study area. At present, the thermal evolution extent of E₂n₂² and E₂n₂³ hydrocarbon source rocks in the Jiangriacuo Sag in the west is the highest, and its hydrocarbon forming and supplying ability is superior to the Jiangjiangcuo and Pacuo sags in the center and east.
- thermal history /
- maturity history /
- source rock /
- Nibao Formation /
- Eocene /
- Lunpola Basin

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