Tapponner P, Xu Z, Roger F, et al. Oblique stepwise rise and growth of the Tibet Plateau[J]. Science,2001, 294 (23):1671~1677.
[4]
Meng Q-R, Hu J-M and Yang F-Z. Timing and magni tude of displacement on the Altyn Tagh fault: constrains from stratigraphic correlation of adjoining Tarim and Qaidam basin,NW China[J]. Terra Nova, 2001, 13(2): 86~91.
Robb L J, Armstrong R A and Waters D J. The history of granulite-facies metamorphism and crustal growth from single zircon U-Pb geochronology: Namaqualand, South Africa[J].Journal of Petrology, 1999, 40(12): 1747~1770.
[8]
Hokada T, Suzuki S, Motoyoshi Y, et al. On the partial melting during UHT metamorphism: Implications from miner al texture, feldspar thermometry and zircon chemistry of the Archaean Napier complex, East Antarctica, AGU[C]. 2000Western Pacific Geophysics Meeting , Abstracts, V31A-03C.2000.
[9]
Dodson M H and McClelland-Brown E. Isotopic and palaeo magnetic evidence for rates of cooling, uplift and erosion[A].In: Snelling N J (ed.). Geochronology and the Geologic Record[C]. Geological Society, London, Memoirs, 1985,10:315~325.
[10]
Searle M P. Geological evidence against large scale pre Holocene offsets along the Karakoram Fault: implications for the limited extrusion of the Tibetan Plateau[J]. Tectonics,1996,15:171~186.
[11]
Pupin J P. Zircon and granite petrology[J]. Contribution to Mineralogy and Petrology, 1980, 73: 207~220.
Amaud N, Delville N, Montel J M, et al. Paleozoic to Cenozoic deformation along the Altyn Tagh fault in the Altun Shan massif area, Eastern Qilian Shan, NE Tibet, China[C].American Geophysical Union Annual Meeting Abstracts,1999, F1018.