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引用本文:陈 刚1 李书恒2 章辉若2 丁 超1 杨 甫1 雷盼盼1. 鄂尔多斯盆地东北部二叠系油气成藏的时间和期次[J]. 中国地质, 2013, 40(5): 1453-1465.
CHEN Gang1, LI Shu-heng2, ZHANG Hui-ruo2, DING Chao1, YANG Fu1, LEI Pan-pan1. Timing and stages of the Permian oil-gas accumulations in northeastern Ordos Basin[J]. Geology in China, 2013, 40(5): 1453-1465(in Chinese with English abstract).
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鄂尔多斯盆地东北部二叠系油气成藏的时间和期次
陈 刚1 李书恒2 章辉若2 丁 超1 杨 甫1 雷盼盼1
作者单位
陈 刚1 李书恒2 章辉若2 丁 超1 杨 甫1 雷盼盼1 1.西北大学 地质学系, 大陆动力学国家重点实验室陕西 西安 7100692.中国石油天然气股份有限公司长庆油田分公司陕西 西安 710021 
摘要:
提要:油气成藏年代学是多旋回叠合盆地油气成藏动力学研究的热点问题。运用钻井岩心样品的自生伊利石同位素定年和流体包裹体间接定年方法,探讨分析了鄂尔多斯盆地东北部二叠系多期次油气成藏的时间和期次。含油气砂岩自生伊利石年龄以较宽的时间域分布在178~108 Ma,测年数据的统计分布特征指示二叠系原生油气成藏时间主要集中在175~155 Ma和145~115 Ma两组主值年龄区间,相应的峰值年龄为165 Ma和130 Ma。流体包裹体测温数据的统计分析与其宿主砂岩磷灰石裂变径迹热史模拟路径的投影关系表明,二叠系不同层段共同经历了与90~78 ℃和125~118 ℃两组统计峰温相应的162~153 Ma和140~128 Ma两期原生油气成藏事件,其中的上二叠统则还经历了统计峰温接近98 ℃、峰值年龄接近30 Ma的一期次生油气成藏事件。由此认为,鄂尔多斯盆地东北部二叠系不同层段在中生代早—中期的多旋回沉降增温过程至少经历了165~153 Ma和140~128 Ma的两期原生油气成藏作用,上二叠统则在晚白垩世以来盆地后期抬升改造阶段的构造动热转换过程经历了接近30 Ma的一期次生油气成藏作用。
关键词:  鄂尔多斯盆地东北部  二叠系砂岩储层  自生伊利石定年  流体包裹体分析  油气成藏年代学
DOI:
分类号:
基金项目:国家973计划(2003CB214607)、国家留学回国人员择优资助与留学基金委西部计划项目(2007127S073)、教育部高校博士点专项科研基金(20116101110006)、陕西省自然科学基金(2012JZ5001)和中国地质调查局油气勘查项目(1212011220761)共同资助。
Timing and stages of the Permian oil-gas accumulations in northeastern Ordos Basin
CHEN Gang1, LI Shu-heng2, ZHANG Hui-ruo2, DING Chao1, YANG Fu1, LEI Pan-pan1
Abstract:
Abstract:Geochronology of oil-gas accumulation (OGA) is a key research frontier for petroleum reservoir-forming dynamics in the multi-cycle superimposed basin. The OGA timing and stages of the Permian reservoirs in northeastern Ordos Basin (OB) are constrained in this paper by K-Ar dating of authigenic illite (AI) and indirect dating of fluid inclusions (FI) from oil-gas-bearing sandstone core samples of the Lower-Upper Permian period. AI dating results of the Permian samples show a wide time span of 178~108 Ma and a spatial decreasing trend from 178~122 Ma in the south to 160-108 Ma in the north. The distribution of the AI ages generally reveals 2-stage primary OGA of the Permian reservoirs, which were mainly developed in the time spans of 175~155 Ma and 145~115 Ma respectively with 2-peak ages of 165 Ma and 130 Ma. Additionally, the FI temperature peaks of the samples and their projected ages on AFT thermal path of the FI-host rocks not only statistically present two groups with a low and a high peak temperatures in ranges of 90~78 °C and 125~118 °C, respectively corresponding to 2-stage primary OGA processes of 162~153 Ma and 140~128 Ma in the Permian reservoirs; nevertheless, there is also a medium temperature group with the peak of 98 °C in agreement with a secondary OGA process of ca. 30 Ma in the Upper Permian reservoirs. An integrated analysis of the AI and FI ages with the regional tectonic thermal evolution reveals that the Permian reservoirs in the northeast OB mainly experienced 2-stage primary OGA processes of 165~153 Ma and 140~128 Ma during the Mid-Early Mesozoic multi-cycle burial heating processes, and then the Upper Permian reservoirs further experienced 1-stage secondary OGA of ca. 30 Ma in accordance with a critical tectonic conversion from the slow to rapid uplift-cooling process during the Late Cretaceous-Neocene period.
Key words:  northeastern Ordos Basin (OB)  Permian sandstone reservoirs  authigenic illite(AI) dating  fluid inclusion (FI) analysis  geochronology of oil-gas accum Ulation (OGA)