| 塔里木盆地北缘阿克苏地区震旦系露头层序地层研究 |
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| 引用本文： | 康建威,牟传龙,周恳恳,王启宇,陈小炜,梁薇,葛祥英.塔里木盆地北缘阿克苏地区震旦系露头层序地层研究[J].沉积与特提斯地质,2016,36(2):47-54. |
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| 作者姓名： | 康建威 牟传龙 周恳恳 王启宇 陈小炜 梁薇 葛祥英 |
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| 作者单位： | 1. 国土资源部沉积盆地与油气资源重点实验室, 四川成都 610081;2. 中国地质调查局成都地质调查中心, 四川成都 610081;3. 成都理工大学, 四川成都 610059 |
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| 基金项目： | 国家重大科技专项"全国油气基础地质编图"(2008ZX05043-005)、中国地质调查局项目"中国岩相古地理编图"(1212010916060) |
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| 摘 要： | 本文对塔里木盆地北缘阿克苏地区磷矿沟震旦系剖面进行了详细的沉积体系研究。结果表明,该剖面主要发育滨岸沉积体系、碎屑岩潮坪沉积体系和碳酸盐潮坪沉积体系,这几种沉积体系的组合反映了震旦纪阿克苏地区由碎屑岩体系向碳酸盐岩体系的演化过程。在野外露头中共识别出4种不同类型的层序界面:(1)海侵上超层序不整合界面;(2)水进侵蚀冲刷面;(3)岩性、岩相转换面;(4)暴露溶蚀面。在识别出层序界面的基础上对震旦系划分出2个二级层序和5个三级层序。第一超层序SS1包含3个三级层序:SQ1、SQ2和SQ3。第二超层序SS2包含2个三级层序组:SQ4和SQ5。
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| 关 键 词： | 阿克苏地区 震旦系 沉积体系 露头层序地层 |
| 收稿时间： | 2015/9/10 0:00:00 |
| 修稿时间： | 2015/12/17 0:00:00 |
Sequence stratigraphic analysis of the Sinian strata in the Aksu region, Xinjiang |
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| KANG Jian-wei,MOU Chuan-long,ZHOU Ken-ken,WANG Qi-yu,CHEN Xiao-wei,LIANG Wei,GE Xiang-ying.Sequence stratigraphic analysis of the Sinian strata in the Aksu region, Xinjiang[J].Sedimentary Geology and Tethyan Geology,2016,36(2):47-54. |
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| Authors: | KANG Jian-wei MOU Chuan-long ZHOU Ken-ken WANG Qi-yu CHEN Xiao-wei LIANG Wei GE Xiang-ying |
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| Institution: | 1. Key Laboratory of Sedimentary Basins and Oil and Gas Resources, Ministry of Land and Resources, Chengdu 610081, Sichuan, China;2. Chengdu Center, China Geological Survey, Chengdu 610081, Sichuan, China;3. Chengdu University of Technology, Chengdu 610059, Sichuan, China |
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| Abstract: | The depositional systems in the Sinian Linkuanggou section in the Aksu region, Xinjiang may fall into the littoral, siliciclastic tidal-flat and carbonate tidal-flat depositional systems. These depositional systems have recorded the evolution from the siliciclastic rock systems to the carbonate rock systems of the Sinian strata in the Aksu region. Four types of sequence boundaries are recognized for the field outcrops, including the transgressive onlap unconformity, transgressive erosional scour surface, lithologic-lithofacies transitional surface and exposure erosional surface. Two second-order sequences and five third-order sequences are also discriminated for the Sinian strata. The supersequence I represented by the Sugaitebulake Formation comprises the sequences SQ1, SQ2 and SQ3, and the supersequence II represented by the Qigebulake Formation comprises the sequences SQ4 and SQ5. The multiphase tectonic movements are interpreted as the major controlling factor for the formation, development and evolution of the sequence stratigraphy. |
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| Keywords: | Aksu region Sinian depositional system outcrop sequence stratigraphy |
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