GEOTHERMOBAROMETRY

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Mineral Chemistry Indicates the Petrogenesis of Rhyolite From The Southwestern Okinawa Trough被引量:4
《Journal of Ocean University of China》2017年第6期1097-1108,共12页CHEN Zuxing ZENG Zhigang WANG Xiaoyuan ZHANG Yuxiang YIN Xuebo CHEN Shuai MA Yao LI Xiaohui QI Hanyan 
supported by the National Key Basic Research Program of China(No.2013CB429700);the National Natural Science Foundation of China(Nos.41325021 and 41306053);the Strategic Priority Research Program of the Chinese Academy of Sciences(No.XDA11030302);the Special Fund for the Taishan Scholar Program of Shandong Province(No.ts201511061);the AoShan Talents Program Supported by Qingdao National Laboratory for Marine Science and Technology(No.2015ASTP-0S17);the Innovative Talent Promotion Program(No.2012RA2191);the Science and Technology Development Program of Shandong Province(No.2013GRC31502);the Scientific and Technological Innovation Project Financially Supported by Qingdao National Laboratory for Marine Science and Technology(No.2015ASKJ03);the National High Level Talent Special Support Program;the CAS/SAFEA International Partnership Program for Creative Research Teams;the Qingdao Collaborative Innovation Center of Marine Science and Technology
To reveal the petrogenesis of rhyolite from the southwestern Okinawa Trough, the mineral chemistry of plagioclase, orthopyroxene, amphibole, quartz and Fe-Ti oxide phenocrysts were analyzed using an electron microprob...
关键词:GEOTHERMOBAROMETRY oxygen FUGACITY XENOCRYSTS MAGMA evolution RHYOLITE OKINAWA Trough 
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