Zircon U–Pb and Hf isotopic study of gneissic rocks from the Chinese Altai: Progressive accretionary history in the early to middle PalaeozoicMin Sun, Alfred Kröner, Chao Yuan et al.|Chemical Geology|2007Cited by 345
Archean crustal evolution of the northern Tarim craton, NW China: Zircon U–Pb and Hf isotopic constraintsXiaoping Long, Aiqin Hu, Chao Yuan et al.|Precambrian Research|2010Cited by 325
Accretionary orogenesis of the Chinese Altai: Insights from Paleozoic granitoidsChao Yuan, Xiaoping Long, Min Sun et al.|Chemical Geology|2007Cited by 304
Detrital zircon ages and Hf isotopes of the early Paleozoic flysch sequence in the Chinese Altai, NW China: New constrains on depositional age, provenance and tectonic evolutionXiaoping Long, Lie‐Wen Xie, Chao Yuan et al.|Tectonophysics|2009Cited by 213
Detrital zircon age and Hf isotopic studies for metasedimentary rocks from the Chinese Altai: Implications for the Early Paleozoic tectonic evolution of the Central Asian Orogenic BeltXiaoping Long, Keda Cai, Min Sun et al.|Tectonics|2007Cited by 213