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埃达克岩的研究现状及其趋势
引用本文:武占祖,陈勇,梁旭辉.埃达克岩的研究现状及其趋势[J].地质找矿论丛,2005,20(3):204-208.
作者姓名:武占祖  陈勇  梁旭辉
作者单位:中国地质大学,资源管理系,武汉,430074;甘肃有色地质勘查局一○六队,兰州,730047;西部矿业股份有限公司,西宁,810000;中国地质大学,资源管理系,武汉,430074
摘    要:达克岩(adakite)是一种中酸性富钠火成岩(安山岩、英安岩、钠质流纹岩及相应的侵入岩),其突出的地球化学特征就是SiO2≥56%,Al2O3≥15%,低重稀土元素(HREE)与Y(如Yb≤1.9×10-6,Y≤18×10-6),高Sr(大多数>400×10-6,La/Yb(≥10.0)与Sr/Y(>20.0~40.0),一般具有正铕异常(少数具有极弱负铕异常).埃达克岩存在两种成因类型:一种由俯冲的年轻(≤25~30Ma)大洋板片熔融形成(O型埃达克岩);另一种由增厚地壳环境中的玄武质下地壳熔融形成(C型埃达克岩).文章从埃达克岩的特征、形成机制、成矿作用、构造背景、动力学意义等几个方面论述了埃达克岩的研究现状,并指出了未来埃达克岩研究的趋势.

关 键 词:埃达克岩  成因类型  板片俯冲  地球动力学意义
文章编号:1001-1412(2005)03-0204-05
收稿时间:2004-06-01
修稿时间:2004-09-28

THE CURRENT SITUATION AND TENDENCY OF RESEARCH ON ADAKITE
WU Zhang-zu,CHENG Yong and LIANG Xu-hui.THE CURRENT SITUATION AND TENDENCY OF RESEARCH ON ADAKITE[J].Contributions to Geology and Mineral Resources Research,2005,20(3):204-208.
Authors:WU Zhang-zu  CHENG Yong and LIANG Xu-hui
Institution:China University of Geoscionces, Wuhan 430074, China;No.106 Team Gansu Non-ferrous Metal Geological prospecting Bureau, Lanzhou 730046, China;Western region mineral industry company, Xining 810000, China;China University of Geoscionces, Wuhan 430074, China
Abstract:Adakite is a kind of intermediate and acid igneous Na-rich rock(andesite, dacite, sodium rhyolite and homologous intrusive rock ) with striking characteristics of SiO2≥56%,Al2O3≥15%,depletion in HREE and Y(Yb≤1.9×10-6,Y≤18×10-6),high Sr(>400×10-6, rarely<400×10-6),La/Yb(≥10.0)and Sr/Y(>20.0-40.0),as well as positive Euranomaly and rare very weak negative Eu aomaly. There are two types of adakites with different petrogenesis:one type is formed by the melting of(≤25-30Ma) subdcted slab(O-type adakite), and the other type is formed by the melting of basaltic lower crust under thickened setting(C-type adakite). The article primarily dicusses the currtent situation on Adakite from the characteristics, mechanism, ore formation, structure background, geodynamics etc. It points out tendency of research on Adakite.
Keywords:adakite  petrogenesis types  subducting slab  geodynamics
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