Volume 39 Issue 2
Feb.  2014
Turn off MathJax
Article Contents
Cao Tingting, Xu Sihuang, Zhou Lian, Wang Yue, 2014. Element Geochemistry Evaluation of Marine Source Rock with High Maturity: A Case Study of Lower Cambrian in Yangba Section of Nanjiang County, Sichuan. Earth Science, 39(2): 199-209. doi: 10.3799/dqkx.2014.019
Citation: Cao Tingting, Xu Sihuang, Zhou Lian, Wang Yue, 2014. Element Geochemistry Evaluation of Marine Source Rock with High Maturity: A Case Study of Lower Cambrian in Yangba Section of Nanjiang County, Sichuan. Earth Science, 39(2): 199-209. doi: 10.3799/dqkx.2014.019

Element Geochemistry Evaluation of Marine Source Rock with High Maturity: A Case Study of Lower Cambrian in Yangba Section of Nanjiang County, Sichuan

doi: 10.3799/dqkx.2014.019
  • Received Date: 2013-05-06
  • Publish Date: 2014-02-01
  • How to evaluate the marine source rocks with high maturity is of crucial importance. Element geochemical indexes are used to build a new evaluating method for source rock in this study. In this paper, the samples are from the Lower Cambrian in Yangba section of Nanjiang County, Sichuan. We used the measured Xxs (a relative excess of X compared to titanium in post-Archean Australian shale), the authigenetic elements from the the same environment are treated as a class. Then, illustrate the linear relation between each of TOC, δ13Ccarb and δ13Corg and the authigenetic elements from the same class, optimize the authigenetic elements that have closely relationship with enriched organic matter. Finally, the factor formula is built to indicate the changing of the quantity and quality of organic matter during the process of formation, deposition and burial according to the factor analysis. This formula is used to divide the rank of source rock quality of the Lower Cambrian in Yangba section. Thus, this geochemistry evaluation method would provide some new ideas for identifying and evaluating the marine high-maturity source rocks.

     

  • loading
  • Alberdi-Genolet, M., Toceo, R., 1999. Trace Metals and Organic Geochemistry of the Machiques Member (Aptian-Albian) and La Luna Formation (Cenomanian-Campanian), Venezuela. Chemical Geology, 160: 19-38. doi: 10.1016/S0009-2541(99)00044-3
    Bailey, S.W., Hornbeck, J.W., Priscoll, C.T., et al., 1996. Calcium Inputs and Transport in a Base Poor Forest Ecosystem as Interpreted by Sr Isotopes. Water Resource Res. , 32: 707-719. doi: 10.1029/95WR03642
    Cao, T.T., Xu, S.H., Wang, Y., et al., 2011. Geobiological Conditions for the Formation of the Lower Cambrian Source Rocks in Yangba Area of Nanjiang County in the Sichuan Basin. Oil & Gas Geology, 32(1): 11-16(in Chinese with English abstract). http://d.wanfangdata.com.cn/periodical/syytrqdz201101002
    Chen, H., Xie, X.N., Li, H.J., et al., 2010. Evaluation of the Permian Marine Hydrocarbon Source Rocks at Shangsi Section in Sichuan Province Using Multi-proxies of Paleoproductivity and Paleoredox. Journal of Palaeogeography, 12(3): 324-333(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GDLX201003011.htm
    Chen, Y.J., Deng, J., Hu, G.X., 1996. Environmental Constraints on the Trace Element Contents and Distribution Patterns in Sediment. Geology and Geochemistry, (3): 97-105(in Chinese).
    Clavert, S.E., 1987. Oceanographic Controls on the Accumulation of Organic Matter in Marine Sediments. In: Brook, J., Fleet, A.J., eds., Marine Petroleum Source Rock. Blackwell Scientific Press, London. doi: 10.1144/GSL.SP.1987.026.01.08
    Hu, X.M., Wang, C.S., Li, X.H., 2001. Stable Carbon Isotope Response to Oceanic Anoxic Events. Journal of Chengdu University of Technology, 28(1): 1-6 (in Chinese with English abstract).
    Huang, J.H., Luo, G.M., Bai, X., et al., 2007. The Organic Fraction of the Total Carbon Burial Flux Deduced from Carbon Isotopes across the Permo-Triassic Boundary at Meishan, Zhejiang Province. Earth Science—Journal of China University of Geosciences, 32(6): 767-773(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX200706007.htm
    Huang, Y.J., Wang, C.S., Wang, Y.L., 2005. Progress in the Study of Proxies of Paleocean Productivity. Earth Science Frontiers, 12(2): 163-170 (in Chinese with English abstract). http://www.researchgate.net/publication/284372158_Progress_in_the_study_of_proxies_of_paleocean_productivity
    Jones, B.J., Manning, A.C., 1994. Comparison of Geochemical Indices Used for the Interpretation of Palaeoredox Conditions in Ancient Mudstones. Palaeogeography, Palaeoclimatology, Palaeoecology, 111(1-4): 111-129. doi: 10.1016/0009-2541(94)90085-X
    Kuypers, M.M., Pancost, R.D., Jaap, S., et al., 1999. A Large and Abrupt Fall in Atmospheric CO2 Concentration during Cretaceous Times. Nature, 399: 342-345. doi: 10.1038/20659
    Li, H.J., Xie, X.N., Huang, J.H., et al., 2012. Main Factors Controlling the Formation of Excellent Marine Source Rocks in Permian Maokou Formation of Northwest Sichuan, China. Earth Science—Journal of China University of Geosciences, 37(1): 171-180 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201201021.htm
    Liu, S.L., Liu, Y.H., Lin, G., et al., 2006. REE Geochemical Characteristics and Geological Significance of Mudstones from Neogene, Nanpu Sag, Bohai Basin. Geoscience, 20(3): 449-456(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ200603012.htm
    Meyers, S.R., Sageman, B.B., Lyons, T.W., 2005. Organic Carbon Burial Rate and the Molybdenum Proxy: Theoretical Framework and Application to Cenomanian-Turonian Oceanic Anoxic Event 2. Paleoceanography, 20: 2002-2020. doi: 10.1029/2004PA001068
    Mi, W.T., Wang, X.L., Feng, Z.Q., et al., 2012. Carbon Isotope Characteristics and the Implication for the Ancient Ocean Evolution of Doushantuo Formation in Weng'an, Guizhou, China. Journal of Chengdu University of Technology (Science & Technology Edition), 39(3): 396-304 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CDLG201203012.htm
    Miller, E.K., Blum, J.D., Friedland, A.J., 1993. Determination of Soil Exchangeable-Cation Loss and Weathering Rates Using Sr Isotope. Nature, 362: 438-441. doi: 10.1038/362438a0
    Taylor, S.R., Mclennan, S.M., 1985. The Continental Crust: It's Composition and Evolution. Blackwell Scientific Press, United States, 25-30. doi: 10.1002/gj.3350210116
    Tenger, Liu, W.H., Xu, Y.C., et al., 2004. The Discussion on Anoxic Environments and Its Geochemical Identifying Indices. Acta Sedimentologica Sinica, 22(2): 365-372 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB200402025.htm
    Tenger, Liu, W.H., Xu, Y.C., et al., 2005a. Correlative Study on Parameters of Inorganic Geochemistry and Hydrocarbon Source Rocks Formative Environment. Advance in Earth Science, 20(2): 193-200(in Chinese with English abstract). http://www.researchgate.net/publication/285837325_Correlative_study_on_parameters_of_inorganic_geochemistry_and_hydrocarbon_source_rocks_formative_environment
    Tenger, Liu, W.H., Xu, Y.C., et al., 2005b. Study on Relation between Inorganic Parameters in Marine Deposits and Developmental Environment of Hydrocarbon Source Rocks: Taking Ordos Basin as an Example. Oil & Gas Geology, 26(4): 411-421. (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYYT200504004.htm
    Tenger, Liu, W.H., Xu, Y.C., et al., 2006. Geochemistry Identification of High-Maturity Marine Carbonate Source Rock—An Example from Ordos Basin. Science in China (Series D), 36(2): 167-176(in Chinese). http://en.cnki.com.cn/Article_en/CJFDTOTAL-JDXG200604005.htm
    Wang, D.R., 2000. The Geochemistry Character of Stable Isotopes of Oil & Gas. Petroleum Industry Press, Beijing (in Chinese).
    Xie, S.C., Yin, H.F., Xie, X.N., et al., 2007. On the Geobiological Evaluation of Hydrocarbon Source Rocks. Earth Science—Journal of China University of Geosciences, 32(6): 727-740(in Chinese with English abstract). http://www.iacademic.info/user-api/na/articleBybaidu?j=61530&a=594556532731777079
    Xu, S.H., Mei, L.F., Yuan, C.P., et al., 2007. Types, Evolution and Pool-Controlling Significance of Pool Fluid Sources in Superimposed Basins: A Case Study from Paleozoic and Mesozoic in South China. Journal of China University of Geosciences, 18(1): 49-59. doi: 10.1016/S1002-0705(07)60018-1
    Zhang, S.C., Wang, R.L., Jin, Z.J., 2006. The Relationship Between the Cambrian-Ordovician High-TOC Source Rock Development and Paleoenvironment Variations in the Tarim Basin, Western China: Carbon and Oxygen Isotope Evidence. Acta Geologica Sinica, 80(3): 459-466(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200603020.htm
    Zhang, Y.G., 2005. Prospection of Petroleum Geochemistry. Petroleum Geology & Experiment, 27(5): 484-489. http://en.cnki.com.cn/Article_en/CJFDTOTAL-SYSD200505009.htm
    Zhao, Z.H., 1997. The Trace Element Geochemistical Principle. Science Press, Beijing (in Chinese).
    Zhou, L., Zhang, H.Q., Wang, J., et al., 2008. Assessment on Redox Conditions and Organic Burial of Siliciferous Sediments at the Latest Permian Dalong Formation in Shangsi, Sichuan, South China. Journal of China University of Geosciences, 19(5): 496-506. doi: 10.1016/S1002-0705(08)60055-2
    曹婷婷, 徐思煌, 王约, 等, 2011. 四川盆地南江杨坝地区下寒武统烃源岩形成的地球生物学条件. 石油与天然气地质, 32(1): 11-16. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201101004.htm
    陈慧, 解习农, 李红敬, 等, 2010. 利用古氧相和古生产力替代指标评价四川上寺剖面二叠系海相烃源岩. 古地理学报, 12(3): 324-333. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201003011.htm
    陈衍景, 邓健, 胡桂兴, 1996. 环境对沉积物微量元素含量和配分型式的制约. 地质地球化学, (3): 97-105. https://www.cnki.com.cn/Article/CJFDTOTAL-DZDQ199603008.htm
    胡修棉, 王成善, 李祥辉, 2001. 大洋缺氧事件的碳稳定同位素响应. 成都理工学院学报, 28(1): 1-6. doi: 10.3969/j.issn.1671-9727.2001.01.001
    黄俊华, 罗根明, 白晓, 等, 2007. 浙江煤山P/ T之交碳同位素对有机碳埋藏的指示意义. 地球科学——中国地质大学学报, 32(6): 767-773. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200706007.htm
    黄永建, 王成善, 汪云亮, 2005. 古海洋生产力指标研究进展. 地学前缘, 12(2): 163-170. doi: 10.3321/j.issn:1005-2321.2005.02.018
    李红敬, 解习农, 黄俊华, 等, 2012. 川西北二叠系茅口组海相优质烃源岩发育控制因素. 地球科学——中国地质大学学报, 37(1): 171-180. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201201021.htm
    刘士林, 刘蕴华, 林舸, 等, 2006. 渤海湾盆地南堡凹陷新近系泥岩稀土元素地球化学特征及其地质意义. 现代地质, 20(3): 449-456. doi: 10.3969/j.issn.1000-8527.2006.03.013
    密文天, 王新利, 冯志强, 等, 2012. 贵州瓮安陡山沱组碳同位素特征及古海洋意义. 成都理工大学学报(自然科学版), 39(3): 396-304. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201203012.htm
    腾格尔, 刘文汇, 徐永昌, 等, 2004. 缺氧环境及地球化学判识标志的探讨——以鄂尔多斯盆地为例. 沉积学报, 22(2): 365-372. doi: 10.3969/j.issn.1000-0550.2004.02.026
    腾格尔, 刘文汇, 徐永昌, 等, 2005a. 无机地球化学参数与有效烃源岩发育环境的相关研究. 地球科学进展, 20(2): 193-200. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ200502008.htm
    腾格尔, 刘文汇, 徐永昌, 等, 2005b. 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. 石油与天然气地质, 26(4): 411-421. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT200504004.htm
    腾格尔, 刘文汇, 徐永昌, 等, 2006. 高演化海相碳酸盐烃源岩地球化学综合判识——以鄂尔多斯盆地为例. 中国科学(D辑), 36(2): 167-176. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200602005.htm
    王大锐, 2000. 油气稳定同位素地球化学. 北京: 石油工业出版社.
    谢树成, 殷鸿福, 解习农, 等, 2007. 地球生物学方法与海相优质烃源岩形成过程的正演和评价. 地球科学——中国地质大学学报, 32(6): 727-740. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200706002.htm
    张水昌, Wang, R.L., 金之钧, 等, 2006. 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. 地质学报, 80(3): 459-466. doi: 10.3321/j.issn:0001-5717.2006.03.020
    张义纲, 2005. 油气地球化学的若干展望. 石油实验地质, 27(5): 484-489. doi: 10.3969/j.issn.1001-6112.2005.05.010
    赵振华, 1997. 微量元素地球化学原理. 北京: 科学出版社.
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Figures(3)  / Tables(3)

    Article views (3531) PDF downloads(515) Cited by()
    Proportional views

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return