吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (1): 53-64.doi: 10.13278/j.cnki.jjuese.20180105

• 大陆架科学钻探 • 上一篇    

南黄海盆地中部隆起CSDP-2井志留系-石炭系岩石学特征及其沉积相

高小惠1,2,3, 张训华3,4, 蔡来星2,3, 郭兴伟2,3, 李文强2,3   

  1. 1. 中国海洋大学海洋地球科学学院, 山东 青岛 266100;
    2. 中国地质调查局青岛海洋地质研究所, 山东 青岛 266071;
    3. 青岛海洋科学与技术试点国家实验室海洋矿产资源评价与探测技术功能实验室, 山东 青岛 266071;
    4. 中国地质调查局南京地质调查中心, 南京 210016
  • 收稿日期:2018-05-14 发布日期:2019-01-18
  • 通讯作者: 蔡来星(1985-),男,在站博士后,主要从事油气地质学方面的研究,E-mail:qingxin717717@126.com E-mail:qingxin717717@126.com
  • 作者简介:高小惠(1984-),女,博士研究生,主要从事海洋地质学方面的研究,E-mail:xueqian_2007@163.com
  • 基金资助:
    国家自然科学基金项目（41776081，41210005）；国家海洋地质专项（DD20160147）；青岛海洋科学与技术试点国家实验室鳌山科技创新计划项目（2015ASKJ03）

Silurian-Carboniferous Petrographic Features and Depositional Facies in the Well CSDP-2 in the Central Uplift of the South Yellow Sea Basin

Gao Xiaohui1,2,3, Zhang Xunhua3,4, Cai Laixing2,3, Guo Xingwei2,3, Li Wenqiang2,3   

  1. 1. College of Marine Geosciences, Ocean University of China, Qingdao 266100, Shandong, China;
    2. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, Shandong, China;
    3. Laboratory for Marine Mineral Resources, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266071, Shandong, China;
    4. Nanjing Center, China Geological Survey, Nanjing 210016, China
  • Received:2018-05-14 Published:2019-01-18
  • Supported by:
    Supported by National Natural Science Foundation of China (41776081,41210005),National Marine Geology Special Project of China (DD20160147) and Aoshan Science and Technology Innovation Project of Pilot National Laboratory for Marine Science and Technology (Qingdao)(2015ASKJ03)

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摘要： 目前，大陆架科学钻探CSDP-2井是南黄海盆地中部隆起上的唯一深钻，是揭示南黄海中-古生界海相地层时代，恢复其沉积环境和构造运动的基准井。本文针对该井开展岩心描述并进行薄片观察，结合测井数据、古生物化石等资料，将志留系-石炭系划分为下志留统高家边组、侯家塘组、坟头组，上泥盆统五通组，下石炭统高骊山组、和州组，上石炭统黄龙组、船山组。其中，志留系沉积了一套浅海陆棚相的细碎屑岩，沉积物以浅海-滨海相砂泥岩为主；泥盆系五通组同样为碎屑岩沉积，稳定的石英砂岩和紫红色泥岩并存，下部为潮坪相，上部则为三角洲相；而石炭系发育台坪、泻湖、颗粒滩等碳酸盐岩台地亚相，岩性以生屑灰岩和泥晶灰岩为主。区域地层对比表明，南黄海盆地中-古生界海相地层是下扬子区由陆域向海域的延伸，其志留系-石炭系岩性序列与下扬子陆域基本一致。

关键词: 大陆架科学钻探, 南黄海盆地, 志留系-石炭系, 岩石学, 沉积环境

Abstract: The Well CSDP-2 of continental shelf drilling program is the only deep well in the central uplift of South Yellow Sea at present, so it has reference value for revealing the Mesozoic-Paleozoic marine stratigraphic epoch and restoring the depositional environment and tectonic movement. Based on the core description and thin-section examination of the rocks,combined with logs and fossils,the Silurian-Carboniferous strata are divided into Lower Silurian Gaojiabian,Houjiatang-and Fentou Forma-tions;Upper Devonian Wutong Formation;Lower Carboniferous Gaolishan-and Hezhou Formations;Upper Carboniferous Huanglong and Chuanshan Formations. Among them,a set of shallow-sea shelf facies with fine clastic rocks were deposited in Silurian. The Devonian Wutong is characterized by the coexistence of stable quartz sandstone and purple red mudstone,with lower tidal flat facies and upper delta facies. Carboniferous is dominated by bioclastic limestone and muddy limestone,mainly developed in platform,lagoon and grain-beach subfacies of carbonate platform. The regional stratigraphic correlation shows that the lithologic sequence of Silurian-Carboniferous is basically consistent with that of the Lower Yangtze land area,indicating that the Mesozoic-Paleozoic marine strata in the South Yellow Sea basin were the extension of the Lower Yangtze platform from land to sea.

Key words: continental shelf drilling program, South Yellow Sea basin, Silurian-Carboniferous, petrology, depositional environment

中图分类号: 

  • P736.2
[1] 张训华,肖国林,吴志强,等. 南黄海油气勘探若干地质问题认识和探讨[M]. 北京:科学出版社,2017. Zhang Xunhua,Xiao Guolin,Wu Zhiqiang,et al. Understanding and Discussion on Some Geological Problems of South Yellow Sea Oil and Gas Exploration[M]. Beijing:Science Press,2017.
[2] 祁江豪,温珍河,张训华,等. 南黄海地区与上扬子地区海相中-古生界岩性地层对比[J]. 海洋地质与第四纪地质,2013,33(1):109-119. Qi Jianghao,Wen Zhenhe,Zhang Xunhua,et al. Lithostratigraphic Correlation of Mesozoic and Palaeozoic Marine Strata Between South Yellow Sea and Upper Yangtze Region[J]. Marine Geology & Quaternary Geology,2013,33(1):109-119.
[3] 蔡峰,熊斌辉. 南黄海海域与下扬子地区海相中-古生界地层对比及烃源岩评价[J]. 海洋地质动态,2007,23(6):1-6. Cai Feng,Xiong Binhui. Comparison of Marine Mesozoic-Paleozoic Strata and Hydrocarbon Source Rocks in the South Yellow Sea and Lower Yangtze Area[J]. Marine Geology Letters,2007,23(6):1-6.
[4] 蔡来星,王蛟,郭兴伟,等. 南黄海中部隆起中-古生界沉积相及烃源岩特征:以CSDP-2井为例[J]. 吉林大学学报(地球科学版),2017,47(4):1030-1046. Cai Laixing,Wang Jiao,Guo Xingwei,et al. Characteristics of Sedimentary Facies and Source Rocks of Mesozoic-Paleozoic in Central Uplift of South Yellow Sea:A Case Study of CSDP-2 Coring Well[J]. Journal of Jilin University (Earth Science Edition),2017,47(4):1030-1046.
[5] 张银国,梁杰. 南黄海盆地二叠系至三叠系沉积体系特征及其沉积演化[J]. 吉林大学学报(地球科学版),2014,44(5):1406-1418. Zhang Yinguo,Liang Jie. Sedimentary System Characteristics and Their Sedimentary Evolution from the Permian to Triassic in the South Yellow Sea Basin[J]. Journal of Jilin University (Earth Science Edition),2014,44(5):1406-1418.
[6] 张训华,杨金玉,李刚,等.南黄海盆地基底及海相中、古生界地层分布特征[J]. 地球物理学报,2014,57(12):4041-4051. Zhang Xunhua,Yang Jinyu,Li Gang,et al. Basement Structure and Distribution of Mesozoic-Paleozoic Marine Strata in the South Yellow Sea Basin[J]. Chinese Journal of Geophysics,2014,57(12):4041-4051.
[7] 张训华. 中国海域构造地质学[M]. 北京:海洋出版社,2008. Zhang Xunhua. Tectonic Geology in China Seas[M]. Beijing:China Ocean Press,2008.
[8] Guo Xingwei,Xu Honghe,Zhu Xiaoqing,et al. Discovery of Late Devonian Plants from the Southern Yellow Sea Borehole of China and Its Palaeogeo-Graphical Implications[J/OL]. Palaeogeography,Palaeoclimatology,Palaeoecology,2017,http://dx.doi.org.10.1016/j.palaeo.2017.08.039.
[9] 郭兴伟,朱晓青,梅西. 大陆架科学钻探首次在南黄海中部隆起钻遇奥陶系地层[J]. 海洋地质与第四纪地质,2017,37(2):66. Guo Xingwei,Zhu Xiaoqing,Mei Xi. The Continental Shelf Drilling Meets Ordovician Strata in the Central Uplift of South Yellow Sea for the First Time[J]. Marine Geology & Quaternary Geology,2017,37(2):66.
[10] 徐学思. 江苏省岩石地层[M]. 武汉:中国地质大学出版社,1997. Xu Xuesi. Lithostratigraphy of Jiangsu Province[M]. Wuhan:China University of Geosciences Press,1997.
[11] 陈旭,袁训来. 华南野外实习指南[M]. 合肥:中国科学技术大学出版社,2013. Chen Xu,Yuan Xunlai. Guide to Field Practice in Southern China[M]. Hefei:China University of Science and Technology Press,2013.
[12] 赵鲁阳,吕大炜,刘海燕,等. 安徽巢北地区五通组沉积环境分析[J]. 沉积学报,2015,33(3):470-479. Zhao Luyang,Lü Dawei,Liu Haiyan,et al. The Analysis on the Depositional Environment of Wutong Formation in Northern Chaohu Area,Anhui[J]. Acta Sedimentologica Sinica,2015,33(3):470-479.
[13] 冯增昭. 沉积岩石学[M]. 北京:石油工业出版社,1991. Feng Zengzhao. Sedimentary Petrology[M]. Beijing:Petroleum Industry Press,1991.
[14] 李双应,金福全. 下扬子盆地石炭纪的岩石学特征及沉积相[J]. 安徽地质,1994,4(3):36-47. Li Shuangying,Jin Fuquan. Carboniferous Petrogra-phic Features and Depositional Facies of the Lower Yangtze Basin[J]. Geology of Anhui,1994,4(3):36-47.
[15] 纪友亮,周勇,王改为,等.下扬子地区古生界海相碳酸盐岩层序地层发育模式及储层预测[J].石油与天然气地质,2011,32(5):724-732. Ji Youliang,Zhou Yong,Wang Gaiwei,et al. Sequence Stratigraphic Models and Reservoir Prediction of the Paleozoic Marine Carbonates in the Lower Yangtze Area[J]. Oil & Gas Geology,2011,32(5):724-732.
[16] 埃里克·弗吕格尔. 碳酸盐岩微相分析、解释及应用[M].马永里,译.2版.北京:地质出版社,2016. Flugel E. Carbonate Microfacies:Analysis,Interpre-tation and Application[M].Translated by Ma Yongli.2nd ed.Beijing:Geological Publishing House,2016.
[17] 江苏省地质调查研究院. 1:25万南京市幅区域地质调查报告[R]. 北京:中国地质调查局,2003. Jiangsu Institute of Geological Survey. Regional Geological Survey Report of 1:250000 Nanjing Area[R]. Beijing:China Geological Survey,2003.
[18] 王鸿祯,楚旭春,刘本培,等.中国古地理图集[M]. 北京:地图出版社,1985. Wang Hongzhen,Chu Xuchun,Liu Benpei,et al. Chinese Palaeogeographic Atlas[M]. Beijing:China Cartographic Publishing House,1985.
[19] 樊隽轩,Melchin M J,陈旭,等. 华南奥陶-志留系龙马溪组黑色笔石页岩的生物地层学[J]. 中国科学:地球科学,2012,42(1):130-139. Fan Junxuan,Melchin M J,Chen Xu,et al. Biostratigraphy and Geography of the Ordovician-Silurian Lungmachi Black Shales in South China[J]. Science China:Earth Sciences,2012,42(1):130-139.
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