Deformation characters and its tectonic evolution of the Southwest Taiwan Basin(台西南盆地构造特征与演化)
通过对南海973航次在该区域的多道地震剖面的解释，并结合重力和磁力资料，发现台西南盆地的主要构造走向为NE-NEE向，沉积上具有独特的双层构造，是一个与南海演化密切相关的新生代伸展型断陷盆地.这个盆地早第三纪开始发育，形成了大量的正断层和由它们控制的一系列半地堑，发育了古新世-渐新世的沉积.渐新世末期盆地受到挤压作用影响，发育了一系列的逆冲断层和反转构造，表明了台西南盆地“先张后挤”的演化特征，从中新世开始进入热力学沉降坳陷发育阶段....
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | zho |
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Zhejiang University Press
2004-03-01
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| Series: | Zhejiang Daxue xuebao. Lixue ban |
| Subjects: | |
| Online Access: | https://doi.org/zjup/1008-9497.2004.31.2.216-220 |
| _version_ | 1797236336782999552 |
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| author | DINGWei-wei(丁巍伟) WANGYu-ming(王渝明) CHENHan-lin(陈汉林) YANGShu-feng(杨树锋) WUNeng-you(吴能有) |
| author_facet | DINGWei-wei(丁巍伟) WANGYu-ming(王渝明) CHENHan-lin(陈汉林) YANGShu-feng(杨树锋) WUNeng-you(吴能有) |
| author_sort | DINGWei-wei(丁巍伟) |
| collection | DOAJ |
| description | 通过对南海973航次在该区域的多道地震剖面的解释，并结合重力和磁力资料，发现台西南盆地的主要构造走向为NE-NEE向，沉积上具有独特的双层构造，是一个与南海演化密切相关的新生代伸展型断陷盆地.这个盆地早第三纪开始发育，形成了大量的正断层和由它们控制的一系列半地堑，发育了古新世-渐新世的沉积.渐新世末期盆地受到挤压作用影响，发育了一系列的逆冲断层和反转构造，表明了台西南盆地“先张后挤”的演化特征，从中新世开始进入热力学沉降坳陷发育阶段. |
| first_indexed | 2024-04-24T17:02:14Z |
| format | Article |
| id | doaj.art-258c3bf6e5a04d17980d22729efc11a4 |
| institution | Directory Open Access Journal |
| issn | 1008-9497 |
| language | zho |
| last_indexed | 2024-04-24T17:02:14Z |
| publishDate | 2004-03-01 |
| publisher | Zhejiang University Press |
| record_format | Article |
| series | Zhejiang Daxue xuebao. Lixue ban |
| spelling | doaj.art-258c3bf6e5a04d17980d22729efc11a42024-03-29T01:58:21ZzhoZhejiang University PressZhejiang Daxue xuebao. Lixue ban1008-94972004-03-01312216220zjup/1008-9497.2004.31.2.216-220Deformation characters and its tectonic evolution of the Southwest Taiwan Basin(台西南盆地构造特征与演化)DINGWei-wei(丁巍伟)0WANGYu-ming(王渝明)1CHENHan-lin(陈汉林)2YANGShu-feng(杨树锋)3WUNeng-you(吴能有)4 1.Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China( 1.浙江大学地球科学系，浙江 杭州 310027) 1.Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China( 1.浙江大学地球科学系，浙江 杭州 310027) 1.Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China( 1.浙江大学地球科学系，浙江 杭州 310027) 1.Department of Earth Sciences, Zhejiang University, Hangzhou 310027, China( 1.浙江大学地球科学系，浙江 杭州 310027) 2.The Marine Geology Survey of Guangzhou, Guangzhou 510075, China( 2.国土资源部广州海洋地质调查局，广东 广州 510075)通过对南海973航次在该区域的多道地震剖面的解释，并结合重力和磁力资料，发现台西南盆地的主要构造走向为NE-NEE向，沉积上具有独特的双层构造，是一个与南海演化密切相关的新生代伸展型断陷盆地.这个盆地早第三纪开始发育，形成了大量的正断层和由它们控制的一系列半地堑，发育了古新世-渐新世的沉积.渐新世末期盆地受到挤压作用影响，发育了一系列的逆冲断层和反转构造，表明了台西南盆地“先张后挤”的演化特征，从中新世开始进入热力学沉降坳陷发育阶段.https://doi.org/zjup/1008-9497.2004.31.2.216-220南海台西南盆地双层构造反转构造构造演化 |
| spellingShingle | DINGWei-wei(丁巍伟) WANGYu-ming(王渝明) CHENHan-lin(陈汉林) YANGShu-feng(杨树锋) WUNeng-you(吴能有) Deformation characters and its tectonic evolution of the Southwest Taiwan Basin(台西南盆地构造特征与演化) Zhejiang Daxue xuebao. Lixue ban 南海 台西南盆地 双层构造 反转构造 构造演化 |
| title | Deformation characters and its tectonic evolution of the Southwest Taiwan Basin(台西南盆地构造特征与演化) |
| title_full | Deformation characters and its tectonic evolution of the Southwest Taiwan Basin(台西南盆地构造特征与演化) |
| title_fullStr | Deformation characters and its tectonic evolution of the Southwest Taiwan Basin(台西南盆地构造特征与演化) |
| title_full_unstemmed | Deformation characters and its tectonic evolution of the Southwest Taiwan Basin(台西南盆地构造特征与演化) |
| title_short | Deformation characters and its tectonic evolution of the Southwest Taiwan Basin(台西南盆地构造特征与演化) |
| title_sort | deformation characters and its tectonic evolution of the southwest taiwan basin 台西南盆地构造特征与演化 |
| topic | 南海 台西南盆地 双层构造 反转构造 构造演化 |
| url | https://doi.org/zjup/1008-9497.2004.31.2.216-220 |
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