ZHANG Ya-feng, PEI Xian-zhi, DING Sa-ping, LI Rui-bao, FENG Jian-yun, SUN Yu, LI Zuo-chen, CHEN You-xin. 2010: LA-ICP-MS zircon U-Pb age of quartz diorite at the Kekesha area of Dulan County, eastern section of the East Kunlun orogenic belt, China and its significance. Geological Bulletin of China, 29(1): 79-85.
    Citation: ZHANG Ya-feng, PEI Xian-zhi, DING Sa-ping, LI Rui-bao, FENG Jian-yun, SUN Yu, LI Zuo-chen, CHEN You-xin. 2010: LA-ICP-MS zircon U-Pb age of quartz diorite at the Kekesha area of Dulan County, eastern section of the East Kunlun orogenic belt, China and its significance. Geological Bulletin of China, 29(1): 79-85.

    LA-ICP-MS zircon U-Pb age of quartz diorite at the Kekesha area of Dulan County, eastern section of the East Kunlun orogenic belt, China and its significance

    • After detailed field survey and indoor analysis, the quartz diorites exposed at the Kekesha area of Dulan, eastern section of the East Kunlun orogenic belt, include four types of rocks: (1)Gray-dark gray medium grained quartz diorite; (2) Gray medium grained gneissic quartz diorite; (3)Gray medium-coarse grained amphibole quartz diorite; (4)Light flesh-red medium-fine grained porphraceous adamellite. LA-ICP-MS method is used to determine the zircon U-Pb isotope age of the rock, which shows that the zircon 206Pb/238U weighted average age of the sample 11013 is 515.2±4.4Ma (MSWD=2.5) and defines the crystallization age of the rocks in Middle Cambrian period. It indicated that East Kunlun orogenic belt had experienced a magmatism event during the early Caledonian.
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