首页|期刊导航|中国地球化学学报（英文版）|Composition of Phengites in Eclogites and Their Retrogressive Derivatives of the Dabieshan Region: Implication for the Applicability of Phengite Geobarometre
中国地球化学学报（英文版）2002，Vol.21Issue(1)：52-56,5.
Composition of Phengites in Eclogites and Their Retrogressive Derivatives of the Dabieshan Region: Implication for the Applicability of Phengite Geobarometre
Composition of Phengites in Eclogites and Their Retrogressive Derivatives of the Dabieshan Region: Implication for the Applicability of Phengite Geobarometre
摘要
Abstract
Phengites in ecologites of the Dabieshan region can be divided into three generations:primary phengite formed during ecologite-facies prograde metamorphism (Phe1), phengite formed during the late stage of eclogite-facies retrograde metamorphism (Phe2) and phengite formedduring amphibolite- to greenschist-facies diaphthoresis (Phe3). Electron microprobe analyses show that the Si and Fe2 + + Mg contents of Phe1 are unexpectedly lower than those of Phe3. Therefore, much caution should be exercised while using the Si content of phengite to estimate the pressure of a retrograde process.关键词
phengite/eclogite/geobarometre/DabieshanKey words
phengite/eclogite/geobarometre/Dabieshan引用本文复制引用
顾连兴,杜建国,翟建平,范建国,赵成浩,张文兰..Composition of Phengites in Eclogites and Their Retrogressive Derivatives of the Dabieshan Region: Implication for the Applicability of Phengite Geobarometre[J].中国地球化学学报（英文版）,2002,21(1):52-56,5.基金项目
This research was financially supported by Key Project No. 9501102-04-01 of Ministry of Geology and Mineral Resources and by State Key Laboratory of Ore Genesis, Nanjing University. （）
