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Zheng Yangdi, Cai Jingong. Characteristics of carbon and oxygen isotopes of carbonate rocks in South Yellow Sea Basin and their implication[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(3): 307-313. doi: 10.11781/sysydz201303307
Citation: Zheng Yangdi, Cai Jingong. Characteristics of carbon and oxygen isotopes of carbonate rocks in South Yellow Sea Basin and their implication[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2013, 35(3): 307-313. doi: 10.11781/sysydz201303307
shu

Characteristics of carbon and oxygen isotopes of carbonate rocks in South Yellow Sea Basin and their implication

doi: 10.11781/sysydz201303307

  • State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

  • Received Date: 2012-08-03
  • Rev Recd Date: 2013-04-17
  • Publish Date: 2013-05-28
    Abstract
  • Based on the analyses of carbon and oxygen isotope composition and palynofacies of carbonate source rocks (P1q-T1q) from the South Yellow Sea Basin,the formation and controlling factors of effective source rocks of marine facies were studied.The correlation between δ13C and δ18O indicated that the carbon and oxygen carbon isotope compositions were similar to those in original ocean.The δ13CPDB values in P1q were heavier than those in T1q,indicating for higher biological productivity,which was favorable for source rock generation.Based on mean value,the δ13CPDB values of P1q were divided into 3 evolution stages corresponding to the changes of palynofacies,indicating that the formation of source rocks varied among different layers.The δ13CPDB values in P1q from well WX5-ST1 were 3.83‰ in average,obviously heavier than those from well CZ24-1-1 (-1.34‰ in average).It corresponded to the high content of amorphous organic matter,and proved the differences of source rock formation among different regions in the same layer.The comparison of carbon and oxygen isotopes and palynofacies showed that the effective matching of biological productivity and preservation condition was favorable for source rock formation.

     

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    • References(25)
  • [1]
    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.
    [2]
    张水昌,张宝民,边立曾,等.中国海相烃源岩发育控制因素[J].地学前缘,2005,12(3):39-48.
    [3]
    Hatch J R,Jacobson S R,Witzke B J,et al.Possible late Middle Ordovician organic carbon isotope excursion:Evidence from Ordovician oils and hydrocarbon source rocks,Mid-Continent and east-central United States[J].AAPG Bulletin,1987,71(11):1342-1354.
    [4]
    Wang K,Chatterton B D E,Wang Y.An organic carbon isotope record of Late Ordovician to Early Silurian marine sedimentary rocks,Yangtze Sea,South China:Implications for CO2 changes during the Hirnantian glaciation[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1997,132(2):147-158.
    [5]
    王大锐,冯晓杰.渤海湾地区下古生界碳氧同位素地球化学研究[J].地质学报,2002,76(3):400-408.
    [6]
    腾格尔,刘文汇,徐永昌,等.海相地层无机参数与烃源岩发育环境的相关研究:以鄂尔多斯盆地为例[J].石油与天然气地质,2005,26(4):411-421.
    [7]
    胡芬.南黄海盆地海相中、古生界油气资源潜力研究[J].海洋石油,2010,30(3):1-8.
    [8]
    范小林.南黄海盆地海相领域油气勘探战略思考[J].海洋油气地质,2001,6(4):35-40.
    [9]
    左景勋,童金南,邱海鸥,等.下扬子地区早三叠世碳酸盐岩碳同位素组成的演化特征[J].中国科学:地球科学,2006,36(2):109-122.
    [10]
    Qing Hairong,Veizer J.Oxygen and carbon isotopic composition of Ordovician brachiopods:implications for coeval seawater[J].Geochimica et Cosmochimica Acta,1994,58(20):4429-4442.
    [11]
    Derry L A,Kaufman A J,Jacobsen S B.Sedimentary cycling and environmental change in the Late Proterozoic:evidence from stable and radiogenic isotopes[J].Geochimica et Cosmochimica Acta,1992,56:1317-1329.
    [12]
    Kaufman A J,Jacobsen S R,Knoll A H.The Vendian record of Sr and C isotopic variations in seawater:implications for tecto-nics and paleoclimate[J].Earth and Planetary Science Letters,1993,120:409-430.
    [13]
    Derry L A,Brasier M D,Corfield R M,et al.Sr and C isotopic in Lower Cambrian carbonates from the Siberian Craton:a paleoenvironmental record during the Cambrian explosion[J].Earth and Planetary Science Letters,1994,128:671-681.
    [14]
    Kaufman A J,Knoll A H,Narbonne G M.Isotopes,ice ages and terminal Proterozoic earth history[J].Preceedings of the National Academy of Sciences of the United States of America,1997,94(3):6600-6605.
    [15]
    Keith M L,Weber J N.Carbon and oxygen isotopic composition of selected limestones and fossils[J].Geochimica et Cosmochimica Acta,1964,28(10/11):1787-1816.
    [16]
    张水昌,WANG R L,金之钧,等.塔里木盆地寒武纪—奥陶纪优质烃源岩沉积与古环境变化的关系:碳氧同位素新证据[J].地质学报,2006,80(3):459-466.
    [17]
    Demaison G J,Moore G T.Anoxic environments and oil source bed genesis[J].AAPG Bulletin,1980,64:1179-1209.
    [18]
    Tyson R V.The genesis and palynofacies characteristics of marine petroleum source rocks[M]//Fleeta J.Marine petroleum source rocks.Oxford:Geological Society Special Publication,1987:47-67.
    [19]
    Lynne E,Ibach J.Relationship between sedimentation rate and total organic carbon content in ancient marine sediments[J].AAPG Bulletin,1982,66:170-188.
    [20]
    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.
    [21]
    Vanaover C L,Humphris S E,Fornari D,et al.Biogeography and ecological setting of Indian Ocean hydrothermal vents[J].Science,2001,294:818-823.
    [22]
    Huc A Y.Paleogeography,Paleoclimate and Source Rocks[M].Tulsa,USA:AAPG,1995.
    [23]
    Müller P J,Suess E.Productivity sedimentation rate and sedimentary organic matter in the oceans-I.Organic carbon preservation//Deep Sea Research Part A.Oceanographic Research Papers.:Elsevier,1979:1347-1362.
    [24]
    Clavert S E.Oceangraphic controls on the accumulation of organic matter in marine sediments//Brook J,Fleet A J,eds.Marine Petroleum Source Rock.London:Blackwell Scientific,1987:137-151.
    [25]
    Pedersen T F,Calvert S E.Anoxia vs productivity:what controls the formation of organic-carbon-rich sediments and sedimentary rock?[J].AAPG Bulletin,1990,74:454-466.
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