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8. 临沧花岗岩带北、南剖面热历史模拟
（a）北侧剖面；（b）南侧剖面；青色线和品红线是关于最冷(蓝线)和最热(红线)样品热史的95%可信区间。AHePRZ: 磷灰石(U-Th)/He部分保存带；ZHePRZ:锆石(U-Th)/He部分保存带；AFTPAZ:磷灰石裂变径迹部分退火带
Fig.8. The thermal histories for the northern transect and southern transect from the Lincang granite belt
（a）Northern transect；（b）Southern transect；The cyan and magenta lines are the 95% credible intervals about the coldest (blue line) and hottest (red line) sample thermal histories．AHePRZ: Apatite He Partial Retention Zone; ZHePRZ: Zircon He Partial Retention Zone; AFTPAZ: Apatite Fission Track Partial Annealing Zone
