Q915.653
国家杰出青年科学基金(编号49625203)，国家计委30届国际地质大会重大项目(编号96-30-14)
日喀则弧前盆地位于拉萨地块与雅鲁藏布江缝合带之间，白垩纪中期沉积一套被称为日喀则群的复理石地层，其构造形态为一东西向延展的复式向斜，主体为是昂仁组，击北两翼的底剖地层分别出露为冲堆组和桑祖岗组。目前我们在复理石沉积中发现了保存较好的以有孔是虫为主的化石群。
The Xigaze Cretaceous forearc basin is situated between the Lhasa Block and Indus-Yarlung Suture. A large suite of flysch was deposited in the basin during the Mid-Cretaceous when the Tethys oceanic crust was being subducted underneath the Eurasian plate.
万晓樵 王成善.1997.西藏日喀则弧前盆地白垩纪有孔虫的发现及年代地层[J].地质学报,71(3):-201,T001.
Wan Xiaoqiao.1997. DISCOVERY OF CRETACEOUS FORAMINIFERA IN THE XIGAZE FOREARC BASIN, XIZANG- WITH A CHRONOSTRATIGRAPHIC DISCUSSION[J]. Acta Geologica Sinica,71(3):-201,T001.
