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《Acta Petrologica Et Mineralogica》 2008-03
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Zircon SHRIMP U-Pb age of quartz diorite in Qagan Obo of Inner Mongolia and its geological significance

ZHANG Wan-yi1,NIE Feng-jun1,JIANG Si-hong1,LIU Yan1,XU Dong-qing1 and GUO Ling-jun2(1.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China;2.Inner Mongolia Geological Survey,Hohhot 010020,China)  
Located in the eastern part of the Baiyinwula-Dong Ujimqin Banner alkali granite belt on the southern edge of the Siberian plate,the Qagan Obo quartz diorite stock has an intimate temporal and spatial relationship with the Qagan Obo Fe-Zn deposit.SHRIMP magmatic zircon U-Pb dating of quartz diorite stock yields an age of 237±6 Ma(1σ),with the MSWD value being 0.63.Based on field geological investigation and laboratory data in combination with the result of zircon dating,it is suggested that the quartz diorite and its associated Fe-Zn ore bodies were formed in Indosinian period.Both of them were formed in a post-collision extensional tectonic setting within the Xing'anling-Mongolia orogenic belt.
【Fund】: 国家自然科学基金资助项目(40573025)
【CateGory Index】: P597.3
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