Geological Relationships Between the Intrusions,Country Rocks,and Ni-Cu-PGE Sulfides of the Kharaelakh Intrusion,Noril′sk Region:Implications for the Roles of Sulfide Differentiation and Metasomatism in Their Genesis

作     者：Peter C.Lightfoot Igor A.Zotov Peter C.Lightfoot;Igor A.Zotov

作者机构：Department of Earth SciencesLaurentian University Institute of Ore Deposit GeologyPetrographyMineralogy and GeochemistryRussian Academy of Sciences Stacomonetnyi pec.35 

出 版 物：《西北地质》 (Northwestern Geology)

年 卷 期：2014年第47卷第1期

页      面：1-35页

学科分类：0709[理学-地质学] 0819[工学-矿业工程] 081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 0708[理学-地球物理学] 0816[工学-测绘科学与技术] 

基　　金：Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits MLR 

主　　题：镁铁质-超镁铁质岩体 铜镍硫化物矿床 成因 kharaelakh诺里尔斯克 交代作用 

摘      要：The Ni-Cu-platinum group element sulfide ore deposits of the Kharaelakh Intrusion,Noril′sk Region,Siberia,represent a large concentration of sulfides associated with a small differentiated intrusion formed at the edge of the Siberian Craton in the roots of the Siberian Trap flood *** deposit is associated with an intrusion that occupies a flanking periclinal structure adjacent to the Noril′sk-Kharaelakh *** intrusion is strongly differentiated and comprises taxitic gabbrodolerites,picritic gabbrodolerites,and gabbrodolerites within the main body which in turn forms a chonolith within a sheet-like intrusion that extends laterally to form extensive undifferentiated sills of *** intrusion substantially replaces the stratigraphy of the country rocks,and although it appears to have exploited the axis of structures developed in response to transtension,the intrusion has created space by both mechanical dilation of stratigraphy and magmatic replacement of pre-existing sedimentary *** frontal lobes of the main intrusion have complex apophyses of gabrodolerite on a range of scales that demonstrate replacement of the sedimentary rocks and link to the development of an extensive metamorphic halo in the country *** halo is much narrower over the main body of the intrusion,and these observations have implications for the thermal history of the ***-skarns and breccias are developed in the roof of the main body of the *** the intrusion,the taxitic rocks contain vesicles and the blebby sulfides developed in the picritic and taxitic gabbrodolerites appear to have a linkage to volatile *** sulfide mineralization developed at the roof of the Kharaelakh Intrusion is associated with metamorphosed and skarn-bearing country rocks,and appears to have been generated by a combination of sulfide fractionation and associated *** geological relationships appear consistent with a chonolith model for the develo