| 新疆吐-哈地区硝酸盐矿床的氧同位素非质量效应 |
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| 引用本文： | 秦燕,李延河,刘锋,侯可军,万德芳.新疆吐-哈地区硝酸盐矿床的氧同位素非质量效应[J].地球学报,2008,29(6):729-734. |
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| 作者姓名： | 秦燕 李延河 刘锋 侯可军 万德芳 |
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| 作者单位： | 中国地质科学院研究生部，北京100037;国土资源部成矿作用与资源评价重点实验室，北京100037；中国地质科学院矿产资源研究所同位素地质重点实验室，北京100037；中国地质科学院矿产资源研究所，北京100037;中国地质科学院研究生部，北京100037;国土资源部成矿作用与资源评价重点实验室，北京100037；中国地质科学院矿产资源研究所同位素地质重点实验室，北京100037；中国地质科学院矿产资源研究所，北京100037;国土资源部成矿作用与资源评价重点实验室，北京100037；中国地质科学院矿产资源研究所同位素地质重点实验室，北京100037；中国地质科学院矿产资源研究所，北京100037 |
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| 基金项目： | 国家自然科学基金项目(编号:40673006,40873003); 国土资源部同位素地质重点实验室、中国地质大学(北京)地质过程与矿产资源国家重点实验室 |
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| 摘 要： | 随着分析测试技术的提高以及同位素分馏理论的进步,氧同位素非质量分馏的应用范围已经从太空拓展到地球,逐渐发展成为研究行星和地球早期演化、地球表面各圈层相互作用的重要途径和手段.硝酸盐和硫酸盐是地球上少数几个具有明显氧同位素非质量分馏效应的矿物.本文测定了新疆吐-哈地区硝酸盐矿床中硝酸盐和硫酸盐矿物的氧同位素组成,结果显示,硝酸盐的氧同位素存在明显的非质量分馏效应,△17O高达14‰,δ18O高达40‰.为该超大型硝酸盐矿床的大气沉积成因提供了可靠依据.
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| 关 键 词： | 氧同位素 非质量效应 硝酸盐 硫酸盐 吐-哈地区 |
Mass Independent Oxygen Isotope Fractionation in Nitrate Deposits of the Turpan-Hami Area, Xinjiang |
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| QIN Yan,LI Yan-he,LIU Feng,HOU Ke-jun and WAN De-fang.Mass Independent Oxygen Isotope Fractionation in Nitrate Deposits of the Turpan-Hami Area, Xinjiang[J].Acta Geoscientia Sinica,2008,29(6):729-734. |
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| Authors: | QIN Yan LI Yan-he LIU Feng HOU Ke-jun and WAN De-fang |
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| Institution: | Graduate School of Chinese Academy of Geological Sciences, Beijing 100037;MRL Key Laboratory of Metallgeny and Mineral Assessment, Beijing 100037; Key Laboratory of Isotope Geology; Institute of Mineral Resources, CAGS, Beijing 100037; Institute of Mineral Resources; Chinese Academy of Geological Science, Beijing 100037;Graduate School of Chinese Academy of Geological Sciences, Beijing 100037;MRL Key Laboratory of Metallgeny and Mineral Assessment, Beijing 100037; Key Laboratory of Isotope Geology; Institute of Mineral Resources, CAGS, Beijing 100037; Institute of Mineral Resources; Chinese Academy of Geological Science, Beijing 100037;MRL Key Laboratory of Metallgeny and Mineral Assessment, Beijing 100037; Key Laboratory of Isotope Geology; Institute of Mineral Resources, CAGS, Beijing 100037; Institute of Mineral Resources; Chinese Academy of Geological Science, Beijing 100037 |
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| Abstract: | With the development of analyzing and measuring techniques and Mass independent isotope fractionation methods,the application of mass independent oxygen isotope fractionation has been used in an increasingly wider field,and has become an important method for studying the evolution of the early earth and the interaction between different circles on the earth.Nitrates and sulfites compose a few existent minerals that have mass independent oxygen isotope fractionation.The authors measured oxygen isotope composition of nitrate and sulfite minerals in the Turpan-Hami Area of Xinjiang, and the results show that there exists obvious mass independent oxygen isotope fractionation in nitrates and slight mass independent oxygen isotope fractionation in sulfites. This paper provides evidence that long-term atmopspheric deposition makes up the sources of superlarge nitrate deposits. |
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| Keywords: | oxygen isotope mass independent fractionation nitrate sulfite Turpan-Hami Area |
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