| Citation: |
Aorigele Zhou, Ju-xing Tang, Ming Zheng, 2020. Eocene uplift and exhumation in Gangdese area: Evidence from zircon U-Pb ages and Al-in-biotite geobarometer, China Geology, 3, 652-655. doi: 10.31035/cg2020073
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Eocene uplift and exhumation in Gangdese area: Evidence from zircon U-Pb ages and Al-in-biotite geobarometer
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References
[1] Ma Y, Xu ZQ, Li GW, Ma SW, Ma XX, Chen XJ, Zhao ZB. 2017. Crustal deformation of the Gangdese Cretaceous back-arc basin and formation of Proto-plateau, South Tibet. Acta Petrologica Sinica, 33(12), 3861–3872 (in Chinese with English abstract). [2] Wang CS, Zhao XX, Liu ZF, Lippert P, Graham S, Coe R, Yi HS, Zhu LD, Liu S, Li YL. 2008. Constraints on the early uplift history of the Tibetan Plateau. PNAS, 105(13), 4987–4992. doi: 10.1073/pnas.0703595105 [3] Uchida E, Endo S, Makino M. 2006. Relationship between solidification depth of granitic rocks and formation of hydrothermal ore deposits. Resource Geology, 51, 47–56. [4] Zhao Z, Lu L, Wu ZH, Hu DG. 2017. Cenozoic uplift process in Gangdese, Tibet: Evidence from thermal history modeling of apatite fission track. Geological Bulletin of China, 36(9), 1553–1561 (in Chinese with English abstract). -
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Aorigele Zhou, Ju-xing Tang, Ming Zheng, 2020. Eocene uplift and exhumation in Gangdese area: Evidence from zircon U-Pb ages and Al-in-biotite geobarometer, China Geology, 3, 652-655. doi: 10.31035/cg2020073
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Figure 1.
Tectonic map of the Tibetan Plateau (a) and geological map of Jiama-Qulong ore concentration district (b); Zircon U-Pb concordance ages (c–e); Al-in-biotite geobarometer data (f).