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, 聂军胜, 郑德文, 庞建章

The Cenozoic Exhumation History and Forcing Mechanism of SE Tibetan Plateau: A Case Study of the Lincang Granite Area
Fangbin LIU, Junsheng NIE, Dewen ZHENG, Jianzhang PANG
表4 临沧花岗岩带磷灰石裂变径迹结果
Table 4 The apatite fission track results of Lincang granite belt
样品Ncρd(Nd)/(×106 cm-2)ρs(Ns)/(×106 cm-2)ρi(Ni)/(×106 cm-2)U/×10-6P(χ2)/%Age±1σ/MaMTL±1SD/μm(Nj)

Dpar±1SD

/μm

YN4193261.206(3 014)1.174(2 653)8.359(18 891)82.29529.8±1.013.50±1.6 (113)2.5±0.21
YN4194151.215(3 036)0.983(703)9.039(6 463)87.867723.3±1.113.22±1.4 (86)2.2±0.15
YN4197291.224(3 058)0.841(1 102)6.966(9 125)67.639526.0±1.113.44±1.4 (45)2.4±0.23
YN4198301.233(3 081)0.658(1 519)5.926(13 688)55.969524.1±0.913.52±1.2 (94)2.1±0.20
YN41910211.242(3 103)1.971(1 620)8.765(7 205)80.129449.1±1.912.95±1.3 (130)2.5±0.22
YN41911281.251(3 126)1.130(1 318)5.449(6 354)51.19045.6±1.913.36±1.5 (50)2.0±0.18