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该区兰片岩于1959年由新疆地质局伊力地质大队首次发现,1974年至1978年新疆地质局区调大队在昭苏县—巩留县所辖哈雷克套山一带开展1∶20万区域地质调查时,在同一地质构造带内多处发现了兰片岩。笔者分别担负了该区区域地质调查和岩矿鉴定工作。在成文过程中,国家地震总局地质研究所冯锦江、张兆忠同志提供了兰闪石X射线粉晶、化学分析成果等资料,并得
The Lanlan schist in the area was first discovered by the Xinjiang Geological Bureau Yili Geological Brigade in 1959. From 1974 to 1978, the Geological Brigade of Xinjiang Uygur Autonomous Region carried out a 1: 200,000 area in the vicinity of Harlech Taoshan under the jurisdiction of Zhaosu-Gongliu County Geological survey, in the same geological structure found in many places blue schist. The author undertook the regional geological survey and rock and mine appraisal respectively. During the writing process, Comrades Feng Jinjiang and Zhang Zhaozhong from the Institute of Geology, State Seismological Bureau provided information on the crystal of amphibole X-ray powder and chemical analysis results, etc.