西永2井铁白云岩Fe同位素地球化学性质及特征

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

    • 摘要: 白云岩发现于200多年前,至今仍然是地球科学研究前沿。西沙群岛白云岩研究超过35 a,发现铁白云岩10 a,属于研究热点。本文在西永2井前期铁白云岩测试研究基础之上,采集典型铁白云岩岩心样品,完成Fe同位素测试,通过对比多种地质储库Fe同位素特征,阐述定位该批测试数据的性质、特征和分析其母源,提出加强投入,与高尖石岛火山岩铁同位素测试结果地球化学特征朔源对比分析的建议。该项研究对于铁白云岩成因特征和机制研究具有重要价值。

       

      Abstract: 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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