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9. 青藏高原东南缘晚始新世（a）、渐新世（b）、中中新世（c）以及现今（d）形变示意图[
LCF: 澜沧江断裂; ALSRR: 哀牢山—红河剪切带
Fig.9. Schematic map showing the deformation in the SE Tibetan Plateau at Late Eocene (a), Oligocene (b), Middle Miocene (c) and present (d)[
LCF: Lancang Fault; ALSRR: Ailao Shan-Red Rvier shear zone
