浙江神仙居流纹质火山岩年代学、地球化学及其地质意义GEOCHRONOLOGY AND GEOCHEMISTRY OF CRETACEOUS RHYOLITES IN THE SHENXIANJU AREA, ZHEJIANG PROVINCE
唐增才,董学发,孟祥随,赵旭东,余盛强,吴小勇,胡开明,陈忠大
摘要(Abstract):
浙江神仙居濒临西太平洋火山岩带,晚中生代构造—岩浆活动频繁,堆积了巨厚的火山沉积地层,是研究晚中生代大陆边缘形成演化动力学过程的重要窗口之一。区内主体为一套流纹质熔结凝灰岩,岩石SiO_2含量为74.17%~78.38%,Al_2O_3含量为11.16%~13.14%,全碱(K_2O+Na_2O)含量为6.44%~8.76%,属高钾钙碱性系列;稀土总量(ΣREE)介于144.5×10~(-6)~247.1×10~(-6)之间,ΣLREE/ΣHREE=5.58~6.81,LaN/YbN=5.17~8.59,δEu为0.17~0.23,弱富集K、Rb,亏损Ba、Sr等大离子亲石元素,相对富集U、Th,亏损Nb、Ta、Ti等高场强元素。LA-ICP-MS锆石U-Pb定年表明,神仙居流纹质熔结凝灰岩同位素年龄集中于(113.4±1.4)Ma~(114.4±1.5)Ma,是早白垩世晚期区域伸展拉张的构造背景下玄武质岩浆底侵作用诱发的地壳部分熔融的产物,层位归属小平田组。
关键词(KeyWords): 化学地层,;锆石LA-ICP-MS U-Pb年龄;地层划分;地球化学;晚中生代;浙江
基金项目(Foundation): 中国地质调查局《浙江区域地质调查片区总结与服务产品开发》(编号:12120114068901);; 浙江省国土资源厅《浙江省中生代火山活动时空演化规律研究》(编号:2017003)项目联合资助
作者(Author): 唐增才,董学发,孟祥随,赵旭东,余盛强,吴小勇,胡开明,陈忠大
DOI: 10.19839/j.cnki.dcxzz.2018.02.005
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