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《Chinese Journal of Geophysics》 2006-01
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Cenozoic cooling history of Lincang granitoid batholith, western Yunnan:Evidence from fission track data

SHI Xiao-Bin~1, QIU Xue-Lin~1, LIU Hai-Ling~1, CHU Zhu-Yin~2,XIA Bin~31 Key Laboratory of Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China2 Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China3 Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China  
To evaluate the history of denudation and cooling of the Lincang granitioid batholith, and investigate the effect of the collision between India and Asia on western Yunnan, zircon and apatite fission track data were obtained on 6 samples from the batholith, and 5 groups of which were used to reveal their temperature-time paths with a nonlinear inversion model, which employs a simulated annealing algorithm. Based on the temperature-time paths, the amount of denudation and uplift was estimated. The results indicate that, since the continent-continent collision of the Indian plate and Asian plate, the batholith has undergone two cooling stages. The cooling rate of the early stage is only 5~10 ℃/Ma,while the cooling rate of the later stage is much larger than that of the early one, especially the rate is up to 16~20 ℃/Ma since 3 Ma B. P.; The total denudation of the two cooling stages is about 3300~3500 m. The analyses also show that the two cooling events are closely related with the collision of India and Asia. The early cooling event is the result from the denudation of the batholith which was involved into thrust-nappe tectonics driven by the middle Eocene-Oligocene India-Asia collision, while the later one is the result from the quick whole uplift and erosion of the batholith, since Pliocena especially since 3 Ma B.P., and the amount of tectonic uplift during this stage is about 672~1263 m. The fission track data also indicate that the southern part of the batholith was affected by the collision event earlier than the middle and northern parts.
【Fund】: 中国科学院知识创新工程项目(KZCX2_SW_117 KZCX2_209).
【CateGory Index】: P588.121;P597.3
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