| 低勘探程度盆地烃源岩热演化及排烃史研究——以东海椒江凹陷为例 |
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| 引用本文： | 仝志刚,赵志刚,杨树春,席小应,郝建荣,喻英梅.低勘探程度盆地烃源岩热演化及排烃史研究——以东海椒江凹陷为例[J].石油实验地质,2012,34(3):319-324. |
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| 作者姓名： | 仝志刚 赵志刚 杨树春 席小应 郝建荣 喻英梅 |
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| 作者单位： | 中海油研究总院, 北京100027 |
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| 摘 要： | 低勘探程度盆地,特别是在海域,钻井稀少且一般位于构造高部位,而盆地中心烃源岩埋藏深,又无钻井揭示,如何评价盆地中心烃源岩的演化程度和排烃历史是盆地或凹陷评价的关键问题。该文以东海椒江凹陷为例,从凹陷边缘或构造高部位具备实测温度和镜质体反射率(Ro)资料的钻井出发,利用正演模拟方法,恢复椒江凹陷岩石圈结构及其演化史,进而模拟整个凹陷古新统烃源岩的热演化史。研究表明,椒江凹陷古新统烃源岩现今最大Ro达到2.8%,为过成熟状态。凹陷总排油量略多于排气量,总排烃量为33×108 m3油当量,主要的排烃期在中新世之前。下一步勘探应在凹陷中部凸起带选择圈闭条件好、且形成于中新世之前的目标进行钻探。
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| 关 键 词： | 烃源岩热演化 正演模拟 岩石圈结构 低勘探程度盆地 东海椒江凹陷 |
| 收稿时间： | 2011-11-15 |
Research on thermal evolution and hydrocarbon expulsion history of source rocks in low-exploration basins:a case study on Jiaojiang Sag, East China Sea Basin |
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| Tong Zhigang
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Zhao Zhigang
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Yang Shuchun
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Xi Xiaoying
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Hao Jianrong
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Yu Yingmei.Research on thermal evolution and hydrocarbon expulsion history of source rocks in low-exploration basins:a case study on Jiaojiang Sag, East China Sea Basin[J].Petroleum Geology & Experiment,2012,34(3):319-324. |
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| Authors: | Tong Zhigang Zhao Zhigang Yang Shuchun Xi Xiaoying Hao Jianrong Yu Yingmei |
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| Affiliation: | Research Institute of CNOOC, Beijing 100027, China |
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| Abstract: | In low-exploration basins,especially offshore ones,wells are rare and usually locate in the higher positions.The source rocks in basin centers are buried deeply and are not drilled.Therefore,it is the key for basin/sag evaluation to study the thermal evolution and hydrocarbon expulsion history of source rocks in basin centers.Case studies have been carried out in the Jiaojiang Sag of the East China Sea Basin.Based on the measured temperature and Ro data collected from wells locating in the sag edge or the higher positions,by means of forward modeling method,the lithosphere structure and thermal history of the Jiaojiang Sag have been recovered,and the thermal history of Paleocene source rocks in the whole sag have been modeled.The results show that the maximum Ro of Paleocene source rocks in the sag is 2.8%,indicating over-mature state.The total amount of oil expulsion is a little bit more than that of gas expulsion,and the amount of hydrocarbon expulsion is 33×108 m3 oil equivalent.Hydrocarbon expulsion mainly took place before Miocene.In the future exploration,the prospects with good traps and were formed before Miocene in the central uplifts should be focused on. |
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| Keywords: | thermal evolution of source rock forward modeling lithosphere structure low-exploration basin Jiaojiang Sag of East China Sea Basin |
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