2021 Vol. 37, No. 6
Article Contents

XU Hong, ZHANG Haiyang, LI Xushen, SHEN Jiangyuan, MA Xiao, FU Heping, ZHANG Daojun, SU Dapeng, YAN Guijing, DONG Gang, LIU Xinyu, YAN Zhuoyu. GEOCHEMICAL BEHAVIORS AND CHARACTERISTICS OF IRON ISOTOPE IN THE FERROAN DOLOMITE FROM WELL XIYONG 2[J]. Marine Geology Frontiers, 2021, 37(6): 1-7. doi: 10.16028/j.1009-2722.2021.002
Citation: XU Hong, ZHANG Haiyang, LI Xushen, SHEN Jiangyuan, MA Xiao, FU Heping, ZHANG Daojun, SU Dapeng, YAN Guijing, DONG Gang, LIU Xinyu, YAN Zhuoyu. GEOCHEMICAL BEHAVIORS AND CHARACTERISTICS OF IRON ISOTOPE IN THE FERROAN DOLOMITE FROM WELL XIYONG 2[J]. Marine Geology Frontiers, 2021, 37(6): 1-7. doi: 10.16028/j.1009-2722.2021.002

GEOCHEMICAL BEHAVIORS AND CHARACTERISTICS OF IRON ISOTOPE IN THE FERROAN DOLOMITE FROM WELL XIYONG 2

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  • The dolomite was discovered more than 200 years ago, and its research is still one of the frontier subjects in Earth Sciences. The study of dolomite on Xisha Islands is over 35 a, and ferroan dolomite was found for 10 a, which are the research hotspots. On the basis of earlier study of dolomites in well Xiyong 2, the core samples of typical ferroan dolomite are further collected for Fe isotope analysis in this study. By comparing characteristics of Fe isotope of various geological reservoirs, the properties, characteristics and the parent sources of the Fe isotope of dolomites from well Xiyong 2 are elaborated. It is suggested to strengthen the investment and correlate the geochemical characteristics with the Fe isotope test results of the volcanic rock samples from the Gajianshi Island. This study is of great value for the study of the genetic characteristics and mechanism of ferroan dolomite.

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  • [1] CHILINGAR G V,YEN T F. Concepts and models of dolomitization[J]. Earth-Science Reviews,1981,17(3):285-286.

    Google Scholar

    [2] WARREN J. Dolomite:occurrence,evolution and economically important associations[J]. Earth-Science Reviews,2000,52(1/3):1-81.

    Google Scholar

    [3] ZENGER D H, DUNHAM J B, ETHINGTON R L. Concepts and models of dolomitization[M]. Tulsa: SEPM Special Publication, 1980, 28: 1-328.

    Google Scholar

    [4] 许红,王修齐,张健,等. 四川盆地震旦系勘探突破与绵阳-长宁拉张槽的特征及对于下扬子区的意义[J]. 海洋地质前沿,2016,32(3):1-6.

    Google Scholar

    [5] 王修齐,许红,宋家荣,等. 高石梯-龙王庙大气田发现与四川盆地震旦-寒武系油气地质特征及成藏[J]. 海洋地质前沿,2016,32(3):24-32.

    Google Scholar

    [6] 许红. 地球化学系统科学Mg-Fe同位素研究: 实验岩石学与白云岩-铁白云岩中Mg-Fe同位素的地球化学行为分析与实践[C]//第七届全国稳定同位素制备与应用技术交流会, 上海, 2020.

    Google Scholar

    [7] XU H,ZHANG W W,WEI K,et al. Ferroan dolomites in Miocene sediments of the Xisha Islands and their genetic model[J]. Chinese Journal of Oceanology and Limnology,2018,36(1):165-180. doi: 10.1007/s00343-018-7136-3

    CrossRef Google Scholar

    [8] 于吉顺, 雷新荣, 张锦化, 等. 矿物 X 射线粉晶鉴定手册(图谱)上册[M]. 武汉: 华中科技大学出版社, 2011.

    Google Scholar

    [9] 许红. “十二五”大型油气田和煤成气重大科技专项《南海新生代生物礁储层对比研究》成果报告[R]. 青岛: 青岛海洋地质研究所, 2015.

    Google Scholar

    [10] 王国忠. 南海珊瑚礁区沉积学[M]. 北京: 海洋出版社, 2001.

    Google Scholar

    [11] 朱祥坤,李志红,赵铁苗,等. 铁同位素的MC-ICP-MS测定方法与地质标准物质的铁同位素组成[J]. 岩石矿物学杂志,2008,27(4):263-272. doi: 10.3969/j.issn.1000-6524.2008.04.001

    CrossRef Google Scholar

    [12] ZHU X K,MAKISHIMA A,GUO Y,et al. High precision measure-ment of titanium isotope ratios by plasma source mass spectrometry[J]. Intenational Journal of Mass Spectrometry,2002,220:321-329.

    Google Scholar

    [13] 唐索寒,朱祥坤,蔡俊军,等. 用于多接收器等离子体质谱铜铁锌同位素测定的离子交换分离方法[J]. 岩矿测试,2006,25(1):5-8. doi: 10.3969/j.issn.0254-5357.2006.01.002

    CrossRef Google Scholar

    [14] ZHU X K,O′NIONS K R,GUO Y L,et al. Secular variation of iron isotopes in north Atlantic Deep Water[J]. Science,2000,287:2000-2002. doi: 10.1126/science.287.5460.2000

    CrossRef Google Scholar

    [15] 朱祥坤,王跃,闫斌,等. 非传统稳定同位素地球化学的创建与发展[J]. 矿物岩石地球化学通报,2013,32(6):651-688.

    Google Scholar

    [16] BLANCKENBURG F V,MAMBERTI M,SCHOENBERG R,et al. The iron isotope composition of microbial carbonate[J]. Chemical Geology,2008,249(1/2):113-128.

    Google Scholar

    [17] 李志红,朱祥坤,唐索寒. 鞍山-本溪地区条带状铁矿的BIF铁同位素特征及其对成矿机理和地球早期海洋环境的制约[J]. 岩石学报,2012,28(11):3545-3558.

    Google Scholar

    [18] BEARD B L,JOLINSON C M,VON-DAMM K V,et al. Iron isotope constraints on Fe cycling and mass balance in oxygenated Earth oceans[J]. Geology,2003,31:629-632. doi: 10.1130/0091-7613(2003)031<0629:IICOFC>2.0.CO;2

    CrossRef Google Scholar

    [19] POITRASSON F,HALLIDAY A N,LEE D C,et al. Iron isotope differences between Earth,Moon,Mars and Vesta as possible records of contrasted accretion mechanisms[J]. Eath and Planetary Science Letters,2004,223(3/4):253-266.

    Google Scholar

    [20] JOHNSON C M,BEARD B L,BEUKES N J,et al. Ancient geochemical cycling in the earth as inferred from Fe isotope studies of banded iron formations from the Transvaal Craton[J]. Contributions to Mineralogy and Petrology,2003,144(5):523-547. doi: 10.1007/s00410-002-0418-x

    CrossRef Google Scholar

    [21] MATTHEWS A,MORGANS-BELL H S,EMMANUEL S,et al. Controls on iron-isotope fractionation in organic-rich sediments (Kimmeridge Clay,Upper Jurassic,Southern England)[J]. Geochimica et Cosmochimica Acta,2004,68(14):3107-3123. doi: 10.1016/j.gca.2004.01.019

    CrossRef Google Scholar

    [22] FROST C D,BLANCKENBURG F V,SCHOENBERG R,et al. Preservation of Fe isotope heterogeneities during diagenesis and metamorphism of banded iron formation[J]. Contributions to Mineralogy and Petrology,2007,153(2):211.

    Google Scholar

    [23] SHARMA M,POLIZZOTTO M,ANBAR A D. Iron isotopes in hot springs along the Juan de Fuca Ridge[J]. Earth and Planetary Science Letters,2001,194(1/2):39-51.

    Google Scholar

    [24] BEARD B L,JOHNSON CM,SKULAN J L,et al. Application of Fe isotopes to tracing the geochemical and biological cycling of Fe[J]. Chemical Gology,2003,195(1/4):87-117.

    Google Scholar

    [25] ROUXEL O,DOBBEK N,LUDDEN J,et al. Iron isotope fractionation during oceanic crust alteration[J]. Chemical Geology,2003,202:155-82. doi: 10.1016/j.chemgeo.2003.08.011

    CrossRef Google Scholar

    [26] SEVERMANN S,JOHNSON C M,BEARD B L,et al. The effect of early diagenesis on the Fe isotope compositions of porewaters and authigenic minerals in continental margin sediments[J]. Geochimica et Cosmochimica Acta,2006,70(8):2006-2022. doi: 10.1016/j.gca.2006.01.007

    CrossRef Google Scholar

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