| 西南地区二叠纪层序地层及海平面变化 |
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| 引用本文： | 覃建雄,曾允孚,陈洪德,田景春,李余生,钱奕中,寿建峰,沈安江.西南地区二叠纪层序地层及海平面变化[J].沉积与特提斯地质,1998,18(1):19-35. |
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| 作者姓名： | 覃建雄 曾允孚 陈洪德 田景春 李余生 钱奕中 寿建峰 沈安江 |
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| 作者单位： | 成都理工学院沉积地质研究所，杭州石油地质研究所 |
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| 摘 要： | 西南地区二叠系可划分为２个二级层序、１１个三级层序，它们代表１１次三级海平面升降旋回，其中有６次可与欧美地区二叠纪海平面变化相对比，它们是伦纳德（Ｌｅｏｎａｒｄｉａｎ）早期、瓜达卢普（Ｇｕａｄａｌｕｐｉａｎ）早期、瓜达卢普（Ｇｕａｄａｌｕｐｉａｎ）晚期、卡赞（Ｋａｚａｎｉａｎ）早期、鞑靼（Ｔａｔａｒｉａｎ）早期和鞑靼（Ｔａｔａｒｉａｎ）晚期的海平面旋回。研究表明，该区二叠纪相对海平面变化作为全球海平面变化和同沉积构造活动相互作用的产物，它与欧美地区乃至联合古陆发展具反向效应，即具有以海侵型碳酸盐沉积序列为典型的主体海平面上升的特点。作者认为显生宙全球海平面旋回曲线的二叠纪部分总体具有两种类型或分支：其一是以海侵型碳酸盐沉积序列为主的反映海平面主体上升的特提斯型或华南型；其二是以海陆过渡—陆相海退沉积序列为主的揭示海平面主体下降的经典型或欧美型。作者强调，全球二叠纪海侵型全球海平面旋回曲线应以西南地区为代表。
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| 关 键 词： | 层序地层 海平面变化 二叠系 西南地区 特提斯型（华南型） 经典型（欧美型） |
Permian sequence stratigraphy and sea-level changes in southwestern China |
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| Qin Jianxiong,Zeng Yunfu,Chen Hongde,Tian Jingehun,Li Yusheng,Qian Yizhong,Shou Jianfeng,Shen Anjiang.Permian sequence stratigraphy and sea-level changes in southwestern China[J].Sedimentary Geology and Tethyan Geology,1998,18(1):19-35. |
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| Authors: | Qin Jianxiong Zeng Yunfu Chen Hongde Tian Jingehun Li Yusheng Qian Yizhong Shou Jianfeng Shen Anjiang |
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| Institution: | Qin Jianxiong Zeng Yunfu Chen Hongde Tian Jingchun Li Yusheng Chengdu University of Technology Qian Yizhong Shou Jianfeng Shen Anjiang Hangzhou Institute of Petroleum Geology |
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| Abstract: | The Permian strata in southwestern China may be divided into two second order sequences and eleven third order sequences representing eleven third order cycles of sea level changes,of which six cycles,i.e.early Leonardian,early Guadalupian,late Guadalupian,early Kazanian,early Tatarian and late Tatarian sea level cycles may be correlated with those in Euramerica.The results of research in this paper show that the Permian relative sea level changes in the study area are dominantly controlled by global sea level changes and synsedimentary tectonism,and reverse to those in Euamerica,even in Pangea,where the sea level changes are characterized by the sea level rises representing the transgressive sedimentary carbonate sequences.Two types or branches may be recognized for the Permian part of the Phanerozoic sea level curves:one is the so called Tethys type or South China type characterized by the sea level rises representing transgressive sedimentary carbonate sequences;another is so called classic type or Euramerica type characterized by the sea level falls representing transitional regressive sedimentary carbonate sequences.The authors contend that the Permian transgressive global sea level curves should be represented by those for South China. |
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| Keywords: | sequence stratigraphy sea level change Permian southwestern China Tethys type (South China type) classic type (Euramerica type) |
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