The Gaojiacun Mafic-Ultramafic Complex(Sichuan,SW China):Neoproterozoic Magmatic Activity at the Western Margin of the Yangtze Craton

作     者：Marian MUNTEANU YAO Yong Allan H. WILSON Gordon CHUNNETT LUO Yaonan ZHAO Qixue 

作者机构：School of Geosciences University of the Witwatersrand Wits 2050 Private Bag 3 Johannesburg South Africa Anglo-Platinum 28 Harrison St. Johannesburg 2001 South Africa Sichuan Bureau of Geology and Mineral Resources No. 25 Section 1 Renminbeilu Chengdu Sichuan 610081 China 

出 版 物：《Acta Geologica Sinica(English Edition)》 (地质学报（英文版）)

年 卷 期：2006年第80卷第5期

页      面：705-723页

核心收录：

学科分类：081803[工学-地质工程] 08[工学] 0708[理学-地球物理学] 0818[工学-地质资源与地质工程] 

基　　金：The research for this work has been funded by Anglo Platinum South African governmental THRIP grant The manuscript benefited from the discussions with Anthony Naldrett (University of Toronto) 

主　　题：China Neoproterozoic ultramafic-mafic rocks cumulate Cu-Ni deposits 

摘      要：The Neoproterozoic Gaojiacun intrusive complex （GIC） is composed of one big intrusion （ca. 9 × 7.5 km） and numerous satellite intrusions, emplaced in the low-grade schists of the Neoproterozoic Yanbian Group. The main intrusion is concentrically zoned, with peridotite bodies ＋ leucogabbroids in its core （inner zone） and the sequence： olivine hornblende gabbronorite - porphyric pyroxene hornblende gabbronorite （transitional zone） - pyroxene hornblende gabbronorite ＋ hornblende gabbro ＋ diorite （outer zone）, towards the margins. The satellite intrusions are composed either of a single rock type （peridotite, gabbro, diorite or granite） or of different rock types （peridotite ＋ diorite ＋ granite）. Upper crustal contamination is evidenced by the occurrence of numerous metamorphic enclaves, migmatites and mixed rocks in the outer zone of the main intrusion and in the satellite intrusions. Hornblende （often oikocrystic） is present in all mafic and ultramafic rocks. Cu-Ni （-PGE） deposits occur in several satellite intrusions, hosted in peridotite. The geochemical and mineralogical features of GIC support the presence of a subduction zone at the western edge of the Yangtze Craton. A feederrelated genesis of the satellite intrusions is inferred.