%0 Journal Article
%T Genetic types, ore-forming age and geodynamic setting of endogenic molybdenum deposits in the eastern edge of Xing-Meng orogenic belt<br>兴蒙造山带东缘内生钼矿床的成因类型、成矿年代及成矿动力学背景
%A SUN JingGui
%A ZHANG Yong
%A XING ShuWen
%A ZHAO KeQiang
%A ZHANG ZengJie
%A BAI LingAn
%A MA YuBo
%A LIU YongSheng
%A <br>孙景贵
%A 张勇
%A 邢树文
%A 赵克强
%A 张增杰
%A 白令安
%A 马玉波
%A 刘勇胜
%J 岩石学报
%D 2012
%I 
%X The eastern edge of Xing-Meng orogenic belt in China, is an important polymetallic metallogenic district, where more than 20 large-, medium- and small-scale Mo deposits have been found in recent years. According to geological features, geochemical characteristics and geochronology, the endogenic molybdenum deposits in the region are divided into porphyry type, contact-metasomatic hydrothermal type and medium-high temperature hydrothermal type. The research results show that porphyry deposits are associated with high-potassium calc-alkaline granitic magmas, while contact-metasomatic hydrothermal deposits are related to calc-alkaline granitic magma and the nature of host rocks. Metallogenic materials possess the characteristic of crust-mantle mixing source. The Mo mineralization in the study area mainly occurred in 195~165Ma and 115~110Ma. The corresponding geodynamic mechanisms responsible for the Mo mineralization in different times may be closely related to the subduction of paleo-Pacific plate and Izanagi plate towards the Eurasia continent, respectively.
%K Endogenic Mo deposit types
%K Ore-forming episodes
%K Geodynamic setting
%K The eastern edge of Xing-Meng orogenic belt<br>内生钼矿类型
%K 成矿期次
%K 成矿动力学背景
%K 兴蒙造山带东缘
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=621CF755B1A341E5&jid=2013B5467E3054B1614CEC199353FCED&aid=E1046AA59652378D27D8CF35703C9A57&yid=99E9153A83D4CB11&vid=D3E34374A0D77D7F&iid=E158A972A605785F&sid=E62D9AFED5C50734&eid=81ED2BA99A995222&journal_id=1000-0569&journal_name=岩石学报&referenced_num=0&reference_num=137