LIU Feng, CAI Jingong, CHEN Aiguo, PENG Xingpeng. ELEMENT GEOCHEMISTRY OF THE CARBONATE SOURCE ROCK OF THE LOWER PERMIAN CHIHSIA FORMATION IN CHAOHU REGION, ANHUI AND THEIR IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2013, 33(6): 121-127. DOI: 10.3724/SP.J.1140.2013.06121
Citation: LIU Feng, CAI Jingong, CHEN Aiguo, PENG Xingpeng. ELEMENT GEOCHEMISTRY OF THE CARBONATE SOURCE ROCK OF THE LOWER PERMIAN CHIHSIA FORMATION IN CHAOHU REGION, ANHUI AND THEIR IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2013, 33(6): 121-127. DOI: 10.3724/SP.J.1140.2013.06121
shu

ELEMENT GEOCHEMISTRY OF THE CARBONATE SOURCE ROCK OF THE LOWER PERMIAN CHIHSIA FORMATION IN CHAOHU REGION, ANHUI AND THEIR IMPLICATIONS

  • 1. Institute of SINOPEC Shanghai Offshore Oil and Gas Company, Shanghai 200120;

  • 2. College of Ocean and Earth Sciences, Tongji University, Shanghai 200092

More Information
  • Received Date: May 27, 2013
  • Revised Date: September 28, 2013
    Graphical Abstract
    • Abstract
  • The Lower Permian carbonate deposits of the Chihsia Formation located in Chaohu, Lower Yangtze are studied in this paper, with emphasis on the relationship between paleoproductivity, redox conditions and the formation of source rock, upon the basis of element geochemistry. The results demonstrate that Ba and TN have evident relations with biological deposition and can be used as a geochemical proxy for paleoproductivity. V/(V+Ni)ratio, as a geochemical proxy to reconstruct the paleoredox, indicates that the Chihsia Formation was formed in an oxygen-deficient environment. The above mentioned proxies suggest that paleoproductivity and paleoredox have close relation with sea level fluctuation. The effective matching of algae productivity and preservation condition made the region favorable for source rock formation while the Chihsia Formation was deposited. High quality source rocks mainly occur in the lower part of the Middle Limestone Member of the Formation.
    • FullText(HTML)
    • References (17)
  • [1]
    腾格尔. 海相地层元素、碳同位素分布与沉积环境和烃源岩发育关系——以鄂尔多斯盆地为例[D]. 兰州:中国科学院兰州地质研究所, 2004.[Tenger. The distribution of Elements, Carbon and Oxygen Isotopes on Marine Strata and Environmental Correlation between they and Hydrocarbon Source Rocks Formation-An Example from Ordovician Basin, China[D]. Lanzhou:Lanzhou Institute of Geology, Chinese Academy of Science, 2004.]
    [2]
    张宝民, 张水昌, 边立曾, 等. 浅析中国新元古-下古生界海相烃源岩发育模式[J]. 科学通报, 2007, 52(增Ⅰ):58-69.[ZHANG Baomin, ZHANG Shuichang, BIAN Lizeng, et al. Development modes of the Neoproterozoic-Lower Palaeozoic marine hydrocarbon source rocks in China[J]. Chin. Sci. Bull., 2007

    , 52(Suppl I):77-91.]
    [3]
    陈践发, 张水昌, 孙省利, 等. 海相碳酸盐岩优质烃源岩发育的主要影响因素[J]. 地质学报, 2006, 80(3):467-472.

    [CHEN Jianfa, ZHANG Shuichang, SUN Xingli, et al. Main factors influencing marine carbonate source rock formation[J]. Acta Geologica Sinica, 2006, 80(3):467-472.]
    [4]
    陈践发, 张水昌, 鲍志东, 等. 海相优质烃源岩发育的主要影响因素及沉积环境[J]. 海相油气地质, 2006, 11(3):49-54.

    [CHEN Jianfa, ZHANG Shuichang, BAO Zhidong, et al. Main sedimentary environments and influencing factor s for development of marine organic-rich source rocks[J]. Marine Origin Petroleum Geology, 2006, 11(3):49-54.]
    [5]
    周堃. 原始海相盆地类型与含油气条件[C]//扬子海相地质与油气. 北京:石油工业出版社, 1993:3-12.[ZHOU Kun. Primary marine basin types and hydrocarbon bearing conditions[C]//Yangtze Marine Geology and Hydrocarbons. Beijing:Petroleum Industry Press, 1993:3

    -12.]
    [6]
    黄永建, 王成善, 汪云亮. 古海洋生产力指标研究进展[J]. 地学前缘, 2005, 12(2):163-170.

    [HUANG Yongjian, WANG Chengshan, WANG Yunliang. Progress in the study of proxies of pale-ocean productivity[J]. Earth Science Frontiers, 2005, 12(2):163-170.]
    [7]
    Pfeifer K, Kasten S, Christian H, et al. Reconstruction of primary productivity from the barium contents in surface sediments of South Atlantic Ocean[J]. Marine Geology, 2001, 177:13-24.
    [8]
    Hatch J R, Leventhal J S. Relationship between inferred redox potential of the depositional environment and geochemistry of the Upper Pennsylvanian (Missourian) Stark Shale Member of the Dennis Limestone, Wabaunsee County, Kansas, USA[J]. Chemical Geology, 1992, 99:65-82.
    [9]
    郭念发, 赵红格, 陈红.下扬子地区海相地层油气赋存条件分析及选区评价[J]. 西北大学学报:自然科学版,2002,32(5):526-530.

    [GUO Nianfa, ZHAO Hongge, CHEN Hong. Oil-gas occurrence conditions and evaluation of chosen belts of the marine strata in Yangtze Area[J]. Journal of Northwest University (Natural Science Edition), 2002, 32(5):526-530.]
    [10]
    刘峰,蔡进功,吕炳全,等. 巢湖地区栖霞组碳酸盐烃源岩的形成及影响因素[J]. 中国科学:地球科学,2011,41(6):873-886.

    [LIU Feng,CAI Jingong,LV Bingquan,et al. Formation and influencing factors of carbonate source rock of the Lower Permian Chihsia Formation in Chaohu region, Anhui Province[J]. Science China:Earth Sciences,2011,41(6):873-886.]
    [11]
    LIU Feng,CAI Jingong,Lü Bingquan,etal. Formation and influencing factors of carbonate source rock of the Lower Permian Chihsia Formation in Chaohu region, Anhui Province[J]. Science China:Earth Sciences,2011,54(12):1926-1939.
    [12]
    Tyson R V. Palynofacies analysis[C]//Applied Micropalaeontology. Dordrecht:Kluwer Academic Publishers, 1993:153-191.
    [13]
    Meyers P A. Preservation of elemental and isotopic source identification of sedimentary organic matter[J]. Chem. Geol., 1994, 114(3/4):289-302.
    [14]
    Milliman J D, Xie Q C, Yang Z S. Transfer of particulate organic carbon and nitrogen from the Yangtze River to the ocean[J]. Am. J. Sci., 1984, 284(7):824-834.
    [15]
    Tan F G, Cai D L, Edmond J M. Carbon isotopic geochemistry of the Changjiang estuary[J]. Estuar Coast Shelf Sci., 1991, 32(4):395-403.
    [16]
    江纳言, 贾蓉芬, 王子玉, 等. 下扬子二叠纪古地理和地球化学环境[M]. 北京:石油工业出版社, 1994.[JIANG Nayan, JIA Rongfen, WANG Ziyu, et al. Permian paleogeography and geochemical environment in Lower Yangtze Region, China[M]. Beijing:Petroleum Industry Press, 1994.]
    [17]
    施春华, 胡瑞忠, 颜佳新. 栖霞组沉积地球化学特征及其环境意义[J]. 矿物岩石地球化学通报, 2004, 23(2):144-148.

    [SHI Chunhua, HU Ruizhong, YAN Jiaxin. Sedimentary geochemistry of the Qixia Formation and its environmental implication[J]. Bulletin of Mineralogy Petrology and Geochemistry, 2004, 23(2):144-148.]
    • Related Articles

Catalog

    Get Citation
    PDF
    XML
    Article views (1722) PDF downloads (9) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    WeChat WeChat
    Order Code Order Code

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return