| 四川盆地西北部二叠系栖霞阶层序地层特征及地质意义 |
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| 引用本文： | 胡笙,谭秀成,罗冰,张本健,张亚,苏成鹏,芦飞凡,李明隆.四川盆地西北部二叠系栖霞阶层序地层特征及地质意义[J].古地理学报,2020,22(6):1109-1126. |
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| 作者姓名： | 胡笙 谭秀成 罗冰 张本健 张亚 苏成鹏 芦飞凡 李明隆 |
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| 作者单位： | 1. 西南石油大学油气藏地质及开发工程国家重点实验室,四川成都 610500;2. 中国石油天然气集团有限公司碳酸盐岩储层重点实验室西南石油大学研究分室,四川成都 610500;3. 中国石油西南油气田分公司勘探开发研究院,四川成都 610041;4. 中国石油西南油气田分公司川西北气矿,四川江油 621700 |
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| 基金项目： | “十三五”国家科技重大专项(编号: 2016ZX05004002-001)资助; |
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| 摘 要： | 基于露头、钻井岩心和测录井资料,采用层序地层学理论与方法,将四川盆地西北部二叠系梁山组+栖霞组作为一个整体予以解剖,识别出梁山组底界面(Ⅰ型)、栖一段与栖二段界面(Ⅱ型)和栖霞组与茅口组界面(Ⅰ型)3个三级层序界面,将中二叠统栖霞阶划分为2个三级层序: 下部的SQ1层序对应梁山组+栖一段,上部的SQ2层序对应栖二段。通过栖霞阶层序地层格架分析,发现栖霞阶地层存在“底超顶削”的充填规律,统计并绘制SQ1与SQ2层序地层厚度等值线图,对研究区栖霞阶SQ1初期和SQ2期构造—古地理格局进行了恢复,在明确SQ2期为栖霞阶主要成滩期的基础上,结合岩溶发育单元及白云岩展布特征,讨论栖霞阶油气储集意义。结果表明:区内栖霞阶存在北西、北东向隆坳分异,汉南隆起、川北隆起、北缘隆起与广元—旺苍凹陷始终控制了区内沉积格局,指出广元—旺苍海槽雏形始于二叠系栖霞阶。研究区岩溶白云岩孔洞型储集层区与环广元—旺苍凹陷周缘的灰岩岩溶型储集层区为有利的勘探区。
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| 关 键 词： | 层序地层 地层充填规律 构造— 古地理格局 地质意义 栖霞阶 四川盆地 |
| 收稿时间： | 2020-03-13 |
Sequence stratigraphic characteristics and geological significance of the Permian Qixia Stage in northwestern Sichuan Basin |
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| Hu Sheng,Tan Xiu-Cheng,Luo Bing,Zhang Ben-Jian,Zhang Ya,Su Cheng-Peng,Lu Fei-Fan,Li Ming-Long.Sequence stratigraphic characteristics and geological significance of the Permian Qixia Stage in northwestern Sichuan Basin[J].Journal of Palaeogeography,2020,22(6):1109-1126. |
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| Authors: | Hu Sheng Tan Xiu-Cheng Luo Bing Zhang Ben-Jian Zhang Ya Su Cheng-Peng Lu Fei-Fan Li Ming-Long |
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| Institution: | 1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu 610500,China;2. Division of Key Laboratory of Carbonate Reservoirs,CNPC,Southwest Petroleum University,Chengdu 610500,China;3. Exploration and Development Research Institute,PetroChina Southwest Oil & Gasfield Company,Chengdu 610041,China;4. Northwest Sichuan Gasfield,PetroChina Southwest Oil & Gasfield Company,Sichuan Jiangyou 621700,China; |
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| Abstract: | Based on outcrops, drilling, cores, and logging data, the Liangshan Formation and Qixia Formation in the northwestern Sichuan region are analyzed using the theory and method of sequence stratigraphy. Three third-order sequence boundaries are identified, including the basal boundary of Liangshan Formation (type Ⅰ), the boundary between Qi 1 Member and Qi 2 Member (type Ⅱ), and the boundary between the Qixia Formation and the Maokou Formation (type Ⅰ). The Middle Permian Qixia Stage can be subdivided into two third-order sequences (from base to top: SQ1 and SQ2). The SQ1 sequence corresponds to the Liangshan Formation and the Qi 1 Member, and the SQ2 sequence corresponds to the Qi 2 Member. Based on the sequence stratigraphic framework reconstruction of the Qixia Stage, the sedimentary filling pattern of the “onlapping at the base and truncation at the top” is discovered. The contour maps of SQ1 and SQ2 sequence stratigraphic thickness are calculated and plotted. Combined with the stratigraphic filling pattern, the tectonic-palaeogeographical framework of the early SQ1 and SQ2 phases of the Qixia Stage, their geological significance is discussed. At the Qixia Stage, the differentiation between uplift and depression occurs in the northwest and northeast trends. The Hannan uplift, the northern Sichuan uplift, the northern margin uplift and the Guangyuan-Wangcang sag have controlled the sedimentary pattern in the study area. It is indicated that prototype of the Guangyuan-Wangcang Trough began in the Middle Permian Qixia Stage. In the study area, the karst cave-type dolostone reservoir and the karst-type limestone reservoir around the Guangyuan-Wangcang sag rim are favorable exploration areas. |
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| Keywords: | sequence stratigraphy sedimentary filling pattern tectonic-palaeogeographic framework geologic significance Qixia Stage northwestern Sichuan Basin |
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