青藏高原东南缘新生代剥露历史及驱动机制探讨：以临沧花岗岩地区为例
刘方斌1,2,3(
), 聂军胜1,2(), 郑德文4, 庞建章5
), 聂军胜1,2(), 郑德文4, 庞建章5
The Cenozoic Exhumation History and Forcing Mechanism of SE Tibetan Plateau： A Case Study of the Lincang Granite Area
Fangbin LIU1,2,3(), Junsheng NIE1,2(), Dewen ZHENG4, Jianzhang PANG5
), Junsheng NIE1,2(), Dewen ZHENG4, Jianzhang PANG5
图2. 临沧花岗岩带磷灰石和锆石(U-Th)/He年龄-eU/有效半径关系图
(a)~(d)北侧剖面；(e)~(h)南侧剖面
Fig.2. AHe and ZHe ages versus effective uranium content [eU] and equivalent sphere radius for two transects from the Lincang granite belt
(a)~(d) Northern transect; (e)~(h) Southern transect
