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- W2366545254 abstract "The age of the felsic tuff interbedded with the Luobusha conglomerates in western Zetang County is reported for the first time in this paper. LA-ICP-MS zircon U-Pb analysis shows that the tuffs were formed at 18.7±0.2Ma, and hence the time of the initial deposition should be about 20 Ma, whereas the LA-ICP-MS zircon U-Pb age of granite underlying the Luobusa conglomerates is 29.9±0.4Ma. The existence of the tuff documents a volcanic activity developed at 18.7±0.2Ma. In combination with geochronologic data from previous work, the authors hold that volcanic activities were developed all along the Yarlung Zangbo suture zone,meaning the re-activation of the suture zone, which is remarkably similar to the potassic-ultrapotassic volcanism along the Gangdise zone in time and space." @default.
- W2366545254 created "2016-06-24" @default.
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- W2366545254 date "2015-01-01" @default.
- W2366545254 modified "2023-10-03" @default.
- W2366545254 title "LA-ICP-MS zircon U-Pb age of the tuffs from the Luobusha conglomerates in southeast Tibet and its implications" @default.
- W2366545254 hasPublicationYear "2015" @default.
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