| 伸展构造盆地的平衡剖面及其构造意义--以松辽盆地南部为例 |
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| 引用本文： | 颜丹平,田崇鲁,孟令波,张建增,周美夫.伸展构造盆地的平衡剖面及其构造意义--以松辽盆地南部为例[J].地球科学,2003,28(3):275-280. |
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| 作者姓名： | 颜丹平 田崇鲁 孟令波 张建增 周美夫 |
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| 作者单位： | [1]教育部岩石图构造、深部过程及探测技术重点实验室，北京100083 [2]石油大学地质科学系，北京102249 [3]吉林油田勘探开发研究院，吉林松原138000 [4]中国地质大学地球科学与资源学院，北京100083 [5]香港大学地球科学系，香港 |
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| 基金项目： | 国家自然科学基金，吉林油田勘探开发科研院项目，40172070，，， |
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| 摘 要： | 挤压构造的平衡地质剖面分析已经广泛应用于造山带构造分析，但伸展构造区的平衡地质剖面分析实例仍然很少．运用盆地分析的技术与方法，分层序或阶段将地质构造依次恢复、地层逐层回剥，并通过在松辽盆地南部吉林两井油田扶余油层4条剖面的实践，复原出不同时代盆地构造与地层发育的连续剖面，揭示出松辽盆地南部主要构造样式是以浅表构造层次的负花状构造及深层剥离断层发育为特征；断层生长指数、盆地的伸展史和伸展量等参数显示，晚白垩世是构造转型的重要阶段，此前主要为走滑构造样式形成阶段，此后则主要为伸展滑脱构造发育阶段．在此基础上，提出松辽盆地具有伸展一走滑双重力学构造性质，可能是一个弧后构造盆地．
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| 关 键 词： | 伸展构造盆地 挤压构造 平衡地质剖面 地质构造 晚白垩世 走滑构造样式 伸展滑脱构造 |
| 文章编号： | 1000-2383(2003)03-0275-06 |
Balanced Geological Section for Extensional Tectonic Basin and Its Implication: An Example from Southern Songliao Basin |
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| YAN Dan-ping ,TIAN Chong-lu,MENG Ling-bo,ZHANG Jian-zeng,ZHOU Mei-fu.Balanced Geological Section for Extensional Tectonic Basin and Its Implication: An Example from Southern Songliao Basin[J].Earth Science-Journal of China University of Geosciences,2003,28(3):275-280. |
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| Authors: | YAN Dan-ping TIAN Chong-lu MENG Ling-bo ZHANG Jian-zeng ZHOU Mei-fu |
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| Institution: | YAN Dan-ping 1,2,TIAN Chong-lu3,MENG Ling-bo4,ZHANG Jian-zeng2,ZHOU Mei-fu5 |
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| Abstract: | The balanced geological section has been widely used for the analysis of orogenic belt, but it is infrequent for extensional basins. In this paper, 4 extensional balanced geological section analysis were practiced in Fuyu oil layer of Liangjing, Jilin oilfield, southern Songliao basin with the technology and method, including deformation history restoration, decompaction and erosion restoration. The structure of different ages and the continuous sedimentary sections have been restored. The results show that the structural styles possess the characteristics of negative flower structure in the shallow level and extensional detachment in deep level. The parameters, including fault growth index, the basin extensional history and fault detachment depth, indicate that Late Cretaceous is an important stage for the structure transferring mainly with a strike-slip style before this time and an extensional structure and detachment after this time. Therefore, a basin model with twin dynamic property and back-arc characters is proposed. |
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| Keywords: | balanced geological section extensional basin deformational history Liangjing oilfield Songliao basin |
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