 | Wang, Qiang, Wyman, Derek A., Li, Zheng-Xiang, Sun, Weidong, Chung, Sun-Lin, Vasconcelos, Paulo M., Zhang, Qiyue, Dong, Han, Yu, Yuanshan, Pearson, N. (2010) Eocene north–south trending dikes in central Tibet: New constraints on the timing of east–west extension with implications for early plateau uplift?. Earth and Planetary Science Letters, 298 (1) 205-216 doi:10.1016/j.epsl.2010.07.046 | Journal (article/letter/editorial) | | l Eocene north–south trending dikes in central Tibet: New constraints on the timing of east–west extension...Chinese Academy of Sciences, Guangzhou 510640, PR China School of Geosciences, Division of Geology and Geophysics...Geology and Mineral Resources, Chengdu 610082, PR China g ARC National Key Centre for Geochemical Evolution...August 2010 Editor: R.D. van der Hilst Keywords: Tibet uplift extension crustal flow dikes global climate...feature of Cenozoic tectonics in central-southern Tibet, and the onset of this extension has been interpreted |  | Wang, Fei, Jourdan, Fred, Lo, Ching-Hua, Nomade, Sebastien, Guillou, Herve, Zhu, Rixiang, Yang, Liekun, Shi, Wenbei, Feng, Huile, Wu, Lin, Sang, Haiqing (2014) YBCs sanidine: A new standard for 40Ar/39Ar dating. Chemical Geology, 388. 87-97 doi:10.1016/j.chemgeo.2014.09.003 | Journal (article/letter/editorial) | | Geophysics, Chinese Academy of Sciences, Beijing 100029, China JdL Centre & Department of Applied Geology Curtin...YBCs, collected from a phonolite at Yabachi in Tibet, China, for single-grain 40Ar/39Ar dating. Aliquots...from the Yabachi volcanic field located in central Tibet (Fig. 1). The Tibetan Plateau comprises the Songpan–Ganzi...aegirine-, riebeckite-, sodalite-, nosean-, hauyne-, leucite-, sanidine- and nepheline-bearing trachytes, phonolites...Located in the west of the Yabachi (Fig. 2), the Yulinshan volcanoes predominantly comprised phonolites and |  | Song, Yucai, Zhang, Chong, Tian, Shihong, Huang, Shiqiang, Zhuang, Liangliang (2016) Mineralization, geochronology, and Pb isotope studies of the shoshonitic lava-hosted Nariniya Pb deposit, central Tibet: linking ore formation to post-collisional potassic magmatism. International Geology Review, 58 (4) 424-440 doi:10.1080/00206814.2015.1086962 | Journal (article/letter/editorial) | | shoshonitic lava-hosted Nariniya Pb deposit, central Tibet: linking ore formation to post-collisional potassic...shoshonitic lavahosted Nariniya Pb deposit, central Tibet: linking ore formation to post-collisional potassic...shoshonitic lava-hosted Nariniya Pb deposit, central Tibet: linking ore formation to post-collisional potassic...Beijing, China; bInstitute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing, China; cChina...cChina University of Geosciences (Beijing), Beijing, China ABSTRACT ARTICLE HISTORY A newly discovered, |  | Zhao, Zhidan, Mo, Xuanxue, Dilek, Yildirim, Niu, Yaoling, DePaolo, Don J., Robinson, Paul, Zhu, Dicheng, Sun, Chenguang, Dong, Guochen, Zhou, Su (2009) Geochemical and Sr–Nd–Pb–O isotopic compositions of the post-collisional ultrapotassic magmatism in SW Tibet: Petrogenesis and implications for India intra-continental subduction beneath southern Tibet. Lithos, 113 (1) 190-212 doi:10.1016/j.lithos.2009.02.004 | Journal (article/letter/editorial) | | post-collisional ultrapotassic magmatism in SW Tibet: Petrogenesis and implications for India intra-continental...intra-continental subduction beneath southern Tibet Zhidan Zhao a,⁎, Xuanxue Mo a,⁎, Yildirim Dilek b, Yaoling...and Mineral Resources, China University of Geosciences, Beijing 100083, China Department of Geology,...Academy of Geological Sciences, Beijing 100037, China b a r t i c l e i n f o Article history: Received...and MgO N 3%) are common and widespread on the Tibet Plateau, where they are closely linked to N–S-trending |  | | Report (issue) | | collision zone. The Aeolian volcanoes along the ? N o CO s: W 173 a«, (U s/ 6 3 3 N u -O ...Urn SI '-5 'o •w C3 G < Uh C3 ■S TD C cd X CO o G c I « I. •c N C3 PU OJD ...-s s .9 CO © © ■O o i« Q- £ XJ £ < o © •— CO © c (/) UJ DC 3 [9. < O) c O) o c •F 03 _o CO (/3 ©...CO O s < Z o © © © c Ip' o C N © © I - ^™i LT...3 LU c © CO © LU lo, i .y o ™ © 0^ 'cl ^ o CL c © 15 ■9 ■ C o o © 2 w -Q 5 .E © jO CO CO -F c i i |
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