Abstract
Geochronological and isotope studies have been carried out for two important plutons in the Central Western Kunlun Belt. U-Pb single grain zircon dating results show that the North Kudi Pluton (404 Ma) was produced near the end of Caledonian; whereas the previously labeled Hercynian Arkarz Mountain Pluton (215 Ma) is either an Indosinian pluton or a product of multiple-phase magmatism. Sm/Nd isotopic data suggest that their sources are quite heterogeneous, and continental crust played an important role during the generation of these two granitic plutons.
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Yuan, C., Sun, M. & Li, J. Two granitic plutons in Central Western Kunlun Belt: Their ages and possible sources. Chin.Sci.Bull. 44, 1807–1810 (1999). https://doi.org/10.1007/BF02886165
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DOI: https://doi.org/10.1007/BF02886165