摘要
The Himalayan peripheral foreland basin developed when India and Asia collided.Previous studies in the Himalayan foreland were mostly concentrated on Neogene continental clastic sedimentation in sub-Himalaya or Paleogene shallow marine sedimentation along Pakistan,India,and Nepal in Lesser Himalaya. The lack of early stage of underfilled。
作者
Xiumian Hu,Jiangang Wang,Luba Jansa,Fuyuan Wu,Jinhai Yu 1.Department of Earth Sciences,Nanjing University,Nanjing 210093,China. 2.Geological Survey of Canada-Atlantic,Dartmouth,N.S.,Canada 3.Institute of Geology and Geophysics,Chinese Academy of Sciences Beijing 100029,China
出处
《地学前缘》
EI
CAS
CSCD
北大核心
2009年第S1期271-272,共2页
Earth Science Frontiers
