苏鲁超高压变质带东海青龙山高压正片麻岩中白云母的^40Ar/^39Ar年代学研究
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P588.345 P533

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国家自然科学基金,国土资源部国土资源大调查项目,国家重点基础研究发展计划(973计划),49973003,2000020190118,G1999075503,,,


40Ar/39Ar Chronological Study of the Muscovite from Qinglongshan High-Pressure Orthogneiss, Donghai County,Su-Lu UHP-Metamorphic Belt
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    摘要:

    作为东海青龙山榴辉岩围岩的高压变质的正片麻岩,其白云母的常规^40Ar/^39Ar年龄和Rb—Sr、Sm—Nd年龄一致,激光微区Ar同位素分析表明,白云母的Ar同位素分布也是均匀的。由此得出的初步结论是:①高压变质的正片麻岩中的白云母中不含过剩Ar,这类矿物可以作为^40Ar/^39Ar同位素测年的对象;②青龙山榴辉岩中的白云母含大量过剩氩,而作为其围岩的超高压正片麻岩中的白云母却不含过剩氩,这一事实证明了榴辉岩中白云母的过剩氩不是来自围岩,而是榴辉岩自身继承的。

    Abstract:

    The conventional 40Ar/39Ar age of muscovite in high-pressure metamorphic orthogneiss, surrounding rocks of the Qinglongshan eclogite, is identical with its Rb-Sr and Sm-Nd ages. The Laser microprobe analysis shows that the argon isotope is evenly distributed in the muscovite. The preliminary conclusion is (1) muscovite in high-pressure metamorphic orthogneiss does not contain excess argon and can be the object for 40Ar/39Ar dating; (2) muscovite in the Qinglongshan eclogite contains large amounts of excess argon while muscovite in its surrounding rocks, i. e. high-pressure orthogneiss, does not contain excess argon. This fact proves that the excess argon of muscovite in eclogite does not come from its country rocks but from its inheritance.

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陈文 李曙光 张彦 刘新宇.2003.苏鲁超高压变质带东海青龙山高压正片麻岩中白云母的^40Ar/^39Ar年代学研究[J].地质论评,49(5):537-543,[DOI].
CHEN Wen, LI Shuguang, ZHANG Yan, LIU Xinyu) Institute of Geology, Chinese Academy of Geological Sciences, Beijing,) Institute of Geology, Geophysics, Chinese Academy of Sciences, Beijing,) The University of Science, Technology of China, Hefei,.2003.40Ar/39Ar Chronological Study of the Muscovite from Qinglongshan High-Pressure Orthogneiss, Donghai County, Su-Lu UHP-Metamorphic Belt[J]. Geological Review,49(5):537-543.

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