ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
普光气藏长兴—飞仙关组碳酸盐岩C、O同位素、微量元素分析及古环境意义
  
关键词:Puguang gas field  Changxing-Feixianguan Formation  carbonate rocks: carbon isotopic  oxygen isotopic  trace elemet  paleo-envionmen
基金项目:中国石油化工股份有限公司项目(编号:G0800-06-ZS-138)
作者单位E-mail
徐立恒 中国石油大学资源信息学院北京 102249 daqing_daruo@sina.com.cn 
陈践发 中国石油大学资源信息学院北京 102249  
李玲 长江大学地球化学系湖北荆州 434023  
马广宇 中国石油大学资源信息学院北京 102249  
刘钰丹 中国石油大学资源信息学院北京 102249  
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摘要:
Carbon, Oxygen Isotope and Trace element Characteristics of Carbonate Rocks in Changxin-Feixianguan Formation of Puguang Gas Pool and Its Palaeoenvironment Significance
      With Wells Puguang 2 and 6 in the Puguang gas field as the research object, the authors used 116 dolomite samples from Changxing-Feixianguan Formation to analyze characteristics of carbonate and oxygen isotopes, judge the ancient seawater salinity and, combined with sedimentary characteristics, study the sedimentary environment. The result shows that d 13C and salt Z is positively correlated with each other. From Member 1 and 2 through Member 3 to Member 4 of Feixiangaun Formation in Well Puguang 2, sedimentary facies experienced the evolutionary process of platform edge shallow facies-restricted platform-evaporate flat, and the salinity, d13C, Sr, P, Ti and Mn values gradually decreased. During the period of Member 1 and 2 of Feixiangaun Formation, d13C, Sr, P, Ti and Mn values were low and the fluctuation was not obvious, suggesting that the variation of the sea level was insignificant. In addition, the elution of fresh water caused the devrease of the salinity. The period of Member 3 of Deixiangaun Formation was in a tidal flat environment with dry and hot climate, during which the fresh water was considerably evaporated, the salinity increased, the d13C, Sr, P, Ti and Mn values increased, the sea level change was obvious and, as a result, the d13C fluctuation was remarkable.The carbon isotope values decreased abruptly at the last stage of the Changxing Formation, which is probably attributed to the death of large quantities of stenohaline organisms at the end of Permian.
XU Li-heng,CHEN Jian-fang,LI Ling,MA Guang-yu,LIU Yu-dan.2009.Carbon, Oxygen Isotope and Trace element Characteristics of Carbonate Rocks in Changxin-Feixianguan Formation of Puguang Gas Pool and Its Palaeoenvironment Significance[J].Acta Geoscientica Sinica,30(1):103-110.
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