| 莺歌海盆地新近纪以来古构造地貌恢复 |
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| 引用本文： | 肖坤泽,童亨茂,杨东辉,李绪生,范彩伟,张宏祥,黄磊.莺歌海盆地新近纪以来古构造地貌恢复[J].石油实验地质,2020,42(2):215-222. |
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| 作者姓名： | 肖坤泽 童亨茂 杨东辉 李绪生 范彩伟 张宏祥 黄磊 |
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| 作者单位： | 1. 中国石油大学(北京) 油气资源与探测国家重点实验室, 北京 102249; |
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| 基金项目： | 国家油气重大专项（2016ZX05024-005-004）和国家自然科学基金项目（41272160）联合资助。 |
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| 摘 要： | 新近系三亚组和梅山组是莺歌海盆地烃源岩发育的重要层系,研究其古构造地貌是预测烃源岩分布和油气资源潜力的基础。应用"构造应力体制保持不变的情况下,盆地内古构造地貌继承性发育"的思想,在确定莺歌海盆地新近纪构造变形应力体制及其演化的基础上,应用"将今论古"和"比例补偿"的思想和方法,分别以盆地现今地貌特征和地层厚度分布为基础资料,并以单井资料确定局部古海水深度作为约束条件,恢复莺歌海盆地新近纪的古构造地貌(古海水深度)。指出莺歌海盆地在三亚组和梅山组沉积时期是半封闭的局限海湾环境,有利于烃源岩的发育;提出古构造地貌研究的新方法——比例补偿法,可应用于其他盆地古构造地貌的恢复。
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| 关 键 词： | 应力体制 古构造地貌 古海水深度 比例补偿 莺歌海盆地 |
| 收稿时间： | 2019-10-24 |
Restoration of Neogene paleo-geomorphology of Yinggehai Basin |
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| XIAO Kunze,TONG Hengmao,YANG Donghui,LI Xusheng,FAN Caiwei,ZHANG Hongxiang,HUANG Lei.Restoration of Neogene paleo-geomorphology of Yinggehai Basin[J].Petroleum Geology & Experiment,2020,42(2):215-222. |
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| Authors: | XIAO Kunze TONG Hengmao YANG Donghui LI Xusheng FAN Caiwei ZHANG Hongxiang HUANG Lei |
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| Affiliation: | 1. State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum(Beijing), Beijing 102249, China;2. College of Geosciences, China University of Petroleum(Beijing), Beijing 102249, China;3. Chengde Central Seismic Station, Hebei Earthquake Agency, Chengde, Hebei 067000, China;4. Zhanjiang Branch, CNOOC, Zhanjiang, Guangdong 524057, China |
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| Abstract: | The Neogene Sanya and Meishan formations are important sequences of source rocks in the Yinggehai Basin. Understanding the paleo-tectonic geomorphology is an important basis for predicting the distribution of source rocks and the potential of oil and gas resources. Based on the rule that "the paleo-tectonic environment develops in the inherited way when tectonic stress system remains unchanged", we applied the idea and method of "the present is the key to the past" and "proportional compensation" to interpret the Neogene tectonic deformation system and its evolution in the Yinggehai Basin. The current geomorphological features and stratigraphic thickness distribution were used with the paleo-sea depth determined from single well data as a constraint to restore the Neogene paleo-geomorphology of the Yinggehai Basin. The Yinggehai Basin was a semi-enclosed confined bay during the deposition of the Sanya and Meishan formations, which was conducive to the development of source rocks. The "proportional compensation" method, which is a new way for paleo-geomorphology restoration, can be applied in other basins. |
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| Keywords: | stress system paleo-tectonic geomorphology paleo-sea depth proportional compensation Yinggehai Basin |
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