节点文献

大别山地区高压—超高压变质岩石的形成机制与折返过程

The Forming Mechamism and the Returning Processes of the HP-UHP Metamorphic Rocks in Dabie Mountains

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 汤加富侯明金

【Author】 Tang Jiafu, Hou Mingjin Anhui Geological Survey, Hefei, Anhui Province, 230001 School of Resources and Environment of Hefei University of Technology, Hefei, Anhui Province, 230009

【机构】 安徽省地质调查院

【摘要】 高压—超高压变质岩石在大别山地区广泛分布。本文在概略介绍其产出地质背景,岩石及矿物标志的基础上,根据大别山地区的降升剥蚀量,并利用热力学原理对其形成深度,压力(高压釜机制)进行了推算,对其形成机制与折返过程作了新的探索。

【Abstract】 It is widely contributed of the High Ultra-high Pressure Metamorphic rocks in Dabie Mountains. It is described on the geological setting, the marks of the petrology and mineralogy of the UHP Metamorphic rocks. According to the estimate of the uplifting and erosion of the Dabie Mountains, and thermodynamics theory, it was evaluated the depth and pressure (high pressure autoclave) of the formed setting of the UHP Metamorphic rocks. Based on all mentioned above, there is a new explanation on the mechanism of formed and the processes of return of the UHP Metamorphic rocks. Keywords: blue schist belt, eclogite bearing coesite belt, "abnormal crustal pressure", "autoclave of high pressure

  • 【会议录名称】 地壳深部压力状态与地质作用学术研讨会论文集
  • 【会议名称】地壳深部压力状态与地质作用学术研讨会
  • 【会议时间】2003-12
  • 【会议地点】中国北京
  • 【分类号】P588.3
  • 【主办单位】国土资源部国际合作与科技司、中国地质学会、中国地质大学(北京)、国家自然科学基金委员会地学部、地质力学专业委员会
节点文献中: 

本文链接的文献网络图示:

本文的引文网络