Continental subduction channel processes: Plate interface interaction during continental collision
作者: YongFei ZhengZiFu ZhaoYiXiang Chen
作者单位: 1CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China
刊名: Chinese Science Bulletin, 2013, Vol.58 (35), pp.4371-4377
来源数据库: Springer Nature Journal
DOI: 10.1007/s11434-013-6066-x
关键词: continental collisionsubduction channelultrahigh-pressure metamorphismdifferential exhumationtectonic melange
英文摘要: Abstract(#br)The study of subduction-zone processes is a key to development of the plate tectonic theory. Plate interface interaction is a basic mechanism for the mass and energy exchange between Earth’s surface and interior. By developing the subduction channel model into continental collision orogens, insights are provided into tectonic processes during continental subduction and its products. The continental crust, composed of felsic to mafic rocks, is detached at different depths from subducting continental lithosphere and then migrates into continental subduction channel. Part of the subcontinental lithospheric mantle wedge, composed of peridotite, is offscrapped from its bottom. The crustal and mantle fragments of different sizes are transported downwards and upwards inside...
全文获取路径: Springer Nature  (合作)
影响因子:1.319 (2012)

  • subduction 俯冲
  • continental 大陆的
  • Continental 大陆牌汽车
  • collision 碰撞
  • interaction 相互酌
  • channel 槽水道
  • during 在的期间
  • interface 界面