| 南黄海盆地中部隆起上古生界沉积环境探讨 |
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| 引用本文： | 蔡来星,郭兴伟,徐朝晖,张晓华,李文强,肖国林,朱晓青,侯方辉. 南黄海盆地中部隆起上古生界沉积环境探讨[J]. 沉积学报, 2018, 36(4): 695-705. DOI: 10.14027/j.issn.1000-0550.2018.124 |
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| 作者姓名： | 蔡来星 郭兴伟 徐朝晖 张晓华 李文强 肖国林 朱晓青 侯方辉 |
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| 作者单位： | 1.中国地质调查局青岛海洋地质研究所, 山东青岛 266071; |
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| 基金项目： | 国家海洋地质专项项目(DD20160147;DD20179393)，国家地质调查专项项目(121201004000150013)，国家自然科学基金项目(41776081;41210005)，青岛市应用基础研究项目(2016239) |
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| 摘 要： | CSDP-2井是大陆架科学钻探计划（CSDP）在南黄海盆地中部隆起实施的第一口连续取芯井，完井深度2 843.18 m，平均取芯率高达97.7%。综合利用该井岩芯、测井、岩石薄片及古生物化石资料，准确识别出南黄海盆地中部隆起上古生界的岩石类型、沉积构造、岩性组合序列等特征，进而探讨研究区沉积环境及其垂向演化规律。研究结果显示:CSDP-2井所钻遇的二叠系、石炭系、泥盆系地层既包含碎屑岩也包含碳酸盐岩，发育了三角洲相、滨岸相、潮坪相、碳酸盐岩台地相、浅海陆棚相等多种沉积相类型；南黄海盆地晚古生代先后经历了两个完整的海侵-海退旋回，自下而上发育碎屑岩浅海-潮坪沉积体系、碳酸盐岩潮坪-潟湖-颗粒滩沉积体系和碎屑岩三角洲沉积体系，反映了研究区由海相向海陆过渡相逐渐演化的沉积充填过程。
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| 关 键 词： | 沉积环境 上古生界 CSDP-2井 南黄海盆地 |
| 收稿时间： | 2018-01-02 |
Depositional Environment of Upper Paleozoic in the Central Uplift of the South Yellow Sea Basin |
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| CAI LaiXing,GUO XingWei,XU ZhaoHui,ZHANG XiaoHua,LI WenQiang,XIAO GuoLin,ZHU XiaoQing,HOU FangHui. Depositional Environment of Upper Paleozoic in the Central Uplift of the South Yellow Sea Basin[J]. Acta Sedimentologica Sinica, 2018, 36(4): 695-705. DOI: 10.14027/j.issn.1000-0550.2018.124 |
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| Authors: | CAI LaiXing GUO XingWei XU ZhaoHui ZHANG XiaoHua LI WenQiang XIAO GuoLin ZHU XiaoQing HOU FangHui |
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| Affiliation: | 1.Qingdao Institute of Marine Geology, China Geological Survey, Qingdao, Shandong 266071, China;2.Qingdao National Laboratory for Marine Science and Technology/Evaluation and Detection Technology Laboratory of Marine Mineral Resources, Qingdao, Shandong 266237, China;3.College of Geosciences, China University of Petroleum(Beijing), Beijing 102249, China |
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| Abstract: | Well CSDP-2 is the first overall coring well implemented by the Continental Shelf Drilling Program (CSDP) in the Central Uplift of the South Yellow Sea Basin, eastern China, whose completion depth is 2 843.18 m and mean drill-core rate is up to 97.7%. Based on the property of cored rocks, logging data, rock thin sections and other test data of Well CSDP-2, it is accurately distinguished in this paper that the rock types, sedimentary structures and lithological association sequences of Upper Paleozoic rocks in the Central Uplift of the South Yellow Sea Basin and then discuss their related sedimentary environments and vertical variations. The Devonian-Carboniferous-Permian strata drilled by Well CSDP-2 contain not only clastic rocks but also carbonate rocks and develop many sedimentary facies including delta, shore, tidal flat, carbonate platform and shallow shelf. In addition, the South Yellow Sea Basin has been experienced 2 completed transgressive-regressive cycles. Controlled by this mechanism, this region developed a clastic depositional system of sea-tidal flat, a carbonate depositional system of tidal flat-lagoon-grain beach, and a delta depositional system from bottom to top, indicating a sedimentary filling process from marine facies to transitional facies. |
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