| 四川广元上寺剖面晚二叠世-早三叠世旋回地层:基于小波分析的P-T界线地质事件探讨 |
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| 引用本文： | 乔彦国,时志强,王艳艳,张彪.四川广元上寺剖面晚二叠世-早三叠世旋回地层:基于小波分析的P-T界线地质事件探讨[J].古地理学报,2012,14(3):403-410. |
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| 作者姓名： | 乔彦国 时志强 王艳艳 张彪 |
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| 作者单位： | 1.成都理工大学沉积地质研究院，四川成都 610059;2.成都理工大学材料与化学化工学院，四川成都 610059 |
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| 摘 要： | 利用小波分析技术,对采集自四川广元上寺剖面上二叠统-下三叠统格里斯巴赫亚阶以碳酸盐岩为主的沉积序列的自然伽马(GR)能谱序列进行深入分析研究,结果表明,该沉积序列很大程度上受到410∶102.5∶42.6∶21.5的米兰科维奇旋回控制.晚二叠世上寺剖面位于古特提斯洋的深水环境,沉积速率较低,平均为5 cm/ka;二叠纪...
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| 关 键 词： | P-T界线 生物大灭绝 米兰科维奇旋回 沉积速率 小波分析 上寺剖面 |
| 收稿时间： | 2011-06-10 |
The Late Permian-Early Triassic cyclostratigraphy in Shangsi section of Guangyuan area, Sichuan Province: Implications for P-T geological event based on wavelet analysis |
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| Qiao Yanguo
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Shi Zhiqiang
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Wang Yanyan
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Zhang Biao.The Late Permian-Early Triassic cyclostratigraphy in Shangsi section of Guangyuan area, Sichuan Province: Implications for P-T geological event based on wavelet analysis[J].Journal of Palaeogeography,2012,14(3):403-410. |
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| Authors: | Qiao Yanguo Shi Zhiqiang Wang Yanyan Zhang Biao |
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| Institution: | 1.Institute of Sedimentary Geology，Chengdu University of Technology，Chengdu 610059，Sichuan;2.College of Materials and Chemistry & Chemical Engineering，Chengdu University of Technology，Chengdu 610059，Sichuan |
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| Abstract: | Based on the analysis of the GR energy spectrum collected from the Upper Permian to Lower Triassic carbonate rocks in Shangsi section at Guangyuan area,Sichuan Province,it was indicated that the sedimentary layers are controlled by Milankovitch cycles,whose scale ratio was 410:102.5:42.6:21.5.During the Late Permian,the Shangsi area was in a deep-water environment of the paleo-Tethys and the deposition rate was low to 5 cm/ka.During the P-T transitional period the tectonic movement was strong and terrestrial and marine fauna experienced mass extinction.At the same time,weathering rate increased sharply because of the acid rain and lack of terrestrial vegetation and mass terrigenous material fluxed into shallow sea in turn,which resulted in a rapid deposition rate of 25 cm/ka in Shangsi section.The rapid rate of deposition displayed a strong influence on marine ecosystems,that is,it restrained the diversity of marine fauna and delayed the resuscitating of marine ecosystems.The cyclicity of the latest Permian sedimentary record was more obvious and stable in Shangsi section.However,the periodicity turned to be labile when it came to the Early Triassic.We concluded that the accelerated deposition rate and deteriorated sedimentary cyclicity were triggered by the turbulent paleoclimate and mussy marine environment.The perturbation of the terrestrial realm contributed to the change of marine conditions,which might be one of the major reasons for the marine ecosystem recovering relatively slowly in the Early Triassic. |
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| Keywords: | P-T boundary mass extinction Milankovitch cycle deposition rate wavelet analysis Shangsi section |
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