New Discovery of Molybdenite in the Dongping Gold Deposit, Hebei Province, China and its Re-Os Geochronological Implications
摘要
<正>Objective The Dongping gold deposit is located on the northern margin of the North China Craton, and is the largest alkaline pluton-related gold deposit in China(Bao et al., 2014), which is characterized by its large amounts of tellurides. The deposit is largely hosted in the Shuiquangou syenitic complex and consists of auriferous quartz veins and disseminated sulfide ores. It has been
引文
Bao,Z.W.,Sun,W.D.,Li,C.J.,and Zhao,Z.H.,2014,U-Pb dating of hydrothermal zircon from the Dongping gold deposit in North China:Constraints on the mineralization processes.Ore Geology Reviews,61:107-119.
Hart,C.J.R.,Goldfarb,R.J.,Qiu,Y.M.,Snee,L.,Miller,L.D.,and Miller,M.L.,2002,Gold deposits of the northern margin of the North China Craton:multiple late Paleozoic-Mesozoic mineralizing events.Mineralium Deposita,37:326-351.
Nie,F.J.,1998,Geology and origin of the Dongping alkalic-type gold deposit,northern Hebei Province,People's Republic of China.Resource Geology,48:139-158.