| 徐州赵圩地区新元古界风暴沉积序列类型及其水深控制 |
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| 引用本文： | 冯乐,窦鲁星,师庆民,江煜波,孙晓倩.徐州赵圩地区新元古界风暴沉积序列类型及其水深控制[J].沉积与特提斯地质,2013,33(2):32-39. |
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| 作者姓名： | 冯乐 窦鲁星 师庆民 江煜波 孙晓倩 |
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| 作者单位： | 中国矿业大学 资源与地球科学学院,江苏 徐州,221116 |
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| 基金项目： | 大学生实践创新训练计划项目 |
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| 摘 要： | 广义的风暴沉积是自然界内外地质营力促使海水产生足够大的漩涡流,对海底及海岸冲蚀形成的一种事件沉积.徐州赵圩地区发育丰富的晚元古代风暴沉积记录,通过野外露头剖面岩性观察与室内整理,划分出7种不同水深的风暴沉积序列类型.根据冲刷面、滞积层、丘状交错层理(HCS)、液化卷曲层理等典型风暴特征,可将这7种序列与浅海陆棚边缘-台地前缘缓斜坡-台前潮上环境的连续沉积相对应.据此分析了风暴沉积序列与水深的关系,并针对本区的沉积特点对风暴沉积成因进行探讨.
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| 关 键 词： | 风暴沉积 新元古代 沉积标志 水深控制 |
| 收稿时间： | 2012/6/6 0:00:00 |
| 修稿时间： | 2012/7/20 0:00:00 |
The Neoproterozoic storm deposits in the Zhaowei region, Xuzhou, Jiangsu: Depositional sequences and their bathymetric controls |
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| FENG Le,DOU Lu-xing,SHI Qing-min,JIANG Yu-bo,SUN Xiao-qian.The Neoproterozoic storm deposits in the Zhaowei region, Xuzhou, Jiangsu: Depositional sequences and their bathymetric controls[J].Sedimentary Geology and Tethyan Geology,2013,33(2):32-39. |
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| Authors: | FENG Le DOU Lu-xing SHI Qing-min JIANG Yu-bo SUN Xiao-qian |
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| Institution: | School of Resources and Geosciences, China University of Mining and Technology, Xuzhou 221116, Jiangsu, China |
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| Abstract: | The Neoproterozoic storm deposits are well developed in the Zhaowei region, Xuzhou, Jiangsu, and may be grouped into seven depositional sequences in different sedimentary environments. These storm deposits are characterized by scour surface, lag deposits, hummocky cross-bedding and liquefied crinkled bedding. The abovementioned seven depositional sequences of the storm deposits may also be corresponded with the continuous deposits in the shallow shelf margin-platform foreslope-platform supratidal environments, and display a close correlation with water depths. Finally a genetic model is proposed for the storm deposits in the Jiayuan Formation. |
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| Keywords: | storm deposit Neoproterozoic sedimentary indicator bathymetric control |
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