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Trace Element and Sulfur Isotope Compositions of Gold-bearing Pyrite from the Zhangjiawa Iron Skarn Deposit,Laiwu District:Implications for Sources of Early Cretaceous Gold Mineralization in the North China Craton 被引量:2
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作者 DUAN Zhuang FU Yangang +6 位作者 LI Chunjia ZHAO Shaorui GAO Mingbo GAO Jilei JIN Lijie LI Siyuan NGO Dac Xuan 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2021年第5期1771-1774,共4页
Objective The Zhangjiawa iron deposit is the largest-tonnage and representative iron skarn deposit,with proven reserves of 290 Mt at an average of 46%Fe(up to>65%),in the Laiwu district,eastern North China Craton(N... Objective The Zhangjiawa iron deposit is the largest-tonnage and representative iron skarn deposit,with proven reserves of 290 Mt at an average of 46%Fe(up to>65%),in the Laiwu district,eastern North China Craton(NCC)(Figs.1 a,b;Duan and Li,2017).Iron mineralization at Zhangjiawa is mainly hosted along a northern contact zone between the Kuangshan dioritic intrusion and Middle Ordovician carbonate rocks that host numerous evaporite intercalations(Figs.1b,c). 展开更多
关键词 CRETACEOUS ORDOVICIAN carbonate
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