High-P and high-T metamorphic rocks in the Jiamusi Massif, NE China
- 作者：Takasu ; A.Li ; W.Guo ; X.Liu ; Y.
- 会议时间：2008-05-01
- 作者单位：Takasu, A.,Li, W.,Guo, X.(Department of Geoscience, Shimane University, Matsue 690-8504, Japan)Liu, Y.(College of Earth Science, Jilin University, Jianshe Str. 2199, Changchun, 130061, Jilin, P.R. China)
- 母体文献：东北亚地区油气地质与矿产资源学术研讨会论文集
- 会议名称：东北亚地区油气地质与矿产资源学术研讨会
- 会议地点：长春
- 主办单位：国土资源部油气资源战略研究中心
- 语种：chi
- 分类号：P5;P3
摘要
@@Previous worksThe Jiamusi Massif is located in the eastern part of the Paleozoic Central Asian Orogenic belt among the Siberian Craton and the North China Craton, and it is surrounded by four major faults, i.e. the Mudanjiang fault, the Jiamusi-Yitong fault, the Dunhua-Mishan fault and Tongjiang fault. The Jiamusi Massif is composed of the Mashan complex and the Heilongjiang complex. The Mashan complex consists mainly of amphibolite to granulite facies metamorphic rocks accompanied by various granitic rocks.