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《Geotectonica Et Metallogenia》 2011-04
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Study on the Orogenic Type Gold Deposits in Eastern Shandong Province

LI Hongkui1,LI Yifan2,GENG Ke1,ZHUO Chuanyuan1,ZHANG Yubo1 and LIANG Taitao1(1.Shandong Province Experimental Institute of Geological Sciences,Key Laboratory of Metallogenic Process and Resource Utilization of Metallic Minerals of Shangdong Province,Jinan 250013,Shandong,China;2.Civil and Hydraulic Institute,Shandong Universty,Jinan 250061,Shandong,China)  
The mineralization during collision orogenesis is an important part of continental dynamic study.Mapping of the tectonic phases(1:500000) was used to study the dispersion,convergence,collision and orogeny of the continental block in Shandong Province.Duringthe mapping of tectonic phases in Shandong Province,we found that there are two important Mesozoic collision events in Eastern Shandong Province——Indosinian and Yanshannian collision.Indosinian collision orogeny was resulted from the subduction of the Yangtze plate beneath North China plate,which led to the formation of the Sulu high pressure-ultra-high pressure metamorphic belt,synorogenic granites and post-orogenic high-alkali syenites;the Yanshannian collision orogeny originated from the transformation of central Asia-Tethyan tectonic region to the coastal Pacific tectonic plate,and the subduction of the Pacific plate,which is demonstrated as three phases of orogeny and extensions in Eastern Shandong Province.Four sets of granitoids associated with orogenesis can be discerned,i.e.,the Linglong gneissic granites of early orogenic period(J3),the Guojialing granodiorite-granite of the middle orogenic period(K1),the Weideshan diorite-granodorite-granite of the late orogenic period,and in the Laoshan A-type granites of the post-orogenic.SHRIMP U-Pb age of the Guojialing orogenic granodiorite-granite assemblage in middle orogenic period is 130~126 Ma,which is closely related to gold mineralization.The ore-forming age of the gold deposits in Eastern Shandong is 120~115 Ma,which basically represents the main ore forming period.Poly-metallic mineralization is closely related to the Weideshan diorite-granodiorite-granite of late orogenic period which is a period of superimposed gold mineralization in the region.Tectonic-magmatic events and gold mineralization are controlled by the interaction of Tethys,Paleo-Asian Ocean and the Pacific tectonic regions.Dynamic background of the gold mineralization was the transition of Mesozoic tectonic regime and lithospheric thinning,which was resulted from the collision bewteen North China plate and Yangtze plate and subduction of the Pacific plate.
【Fund】: 全国矿产资源潜力评价项目之山东省成矿地质背景研究(编码:1212010813014-01)的成果
【CateGory Index】: P618.51
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