| 皮亚曼背斜形成的古地磁研究 |
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| 引用本文： | 邓云山,孟自芳,康键,丁兆海.皮亚曼背斜形成的古地磁研究[J].新疆地质,1999(2). |
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| 作者姓名： | 邓云山 孟自芳 康键 丁兆海 |
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| 作者单位： | 中国科学院兰州地质研究所，中国石油学会 |
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| 摘 要： | 皮亚曼背斜两翼下二叠统原生剩磁的同褶皱检验结果表明原生剩磁主要是同沉积剩磁，其结果显示，皮亚曼背斜开始发育的时间不晚于早二叠世。从东邻杜瓦地区采集的下二叠统古地磁样品，对测试统计结果经同褶皱检验后得出同样的结论。
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| 关 键 词： | 皮亚曼背斜 剩磁 同褶皱检验 |
PALEOMAGNETIC STUDY ON THE FORMATION OF PIYAMAN ANTICLINE |
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| DENG Yun,shan,MENG Zi fang \ KANG Jian \ DING Zhao hai.PALEOMAGNETIC STUDY ON THE FORMATION OF PIYAMAN ANTICLINE[J].Xinjiang Geology,1999(2). |
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| Authors: | DENG Yun shan MENG Zi fang \ KANG Jian \ DING Zhao hai |
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| Institution: | DENG Yun
shan 1 MENG Zi fang 1 \ KANG Jian 2\ DING Zhao hai 1 |
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| Abstract: | The synfold examination of Lower Permian remanent magnetization from the two
limbs of Piyaman anticline shows that the primary remanent magnetization is mainly the
synsedimentary remanent magnetization,the result indicates that the development of Piyaman
anticline began not later than Early Permian.After synfold examination,the measurement and
statistics of the samples collected from Lower Pemian of east neighboring Duwa regiion reachs
a same conclusion. |
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| Keywords: | Piyaman anticline remanent magnetization synfold examination |
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