初论雪峰山地区基性-超基性岩镍钴铜金矿找矿方向
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摘要
近年来,雪峰山地区的基性-超基性岩矿床找矿工作取得了一定的进展。为了及时总结成矿规律,指导进一步的找矿工作,本文在大量野外调研的基础上,系统总结了该地区基性-超基性岩岩体的地质特征、已有找矿进展的长界镍矿和字溪金矿地质特征及已发现的镍钴铜金等矿化特征,并与国内外同类型矿床的成矿特征进行了比较,最后提出了如下认识:雪峰山地区具备找寻基性-超基性岩矿床潜力,目标矿种主要为镍、钴、铜及金矿,主要矿床类型为岩浆硫化物型镍钴铜矿及蚀变热液型金矿。前者目标地质体以通道-洪江-中方-古丈一带新元古代基性-超基性岩群/带最为有利,后者则以隘口岩群及艾头坪-大洪山岩群的大洪山段最为有利。
A certain progress for prospecting ore deposits related to mafic-ultramafic rocks in the Xuefengshan region has been made recently. Based on a large volume of field investigation,we have systematically summarized the geological and mineralization characteristics of the Changjie Ni ore deposit,the Zixi Au ore deposit,some Ni-Co-Cu-Au mineral occurrences,and the host mafic-ultramafic intrusions,in order to summarize metallogenic regulations and to guide further prospecting work in the area. Moreover,the metallogenic characteristics of Ni-Co-Cu-Au deposits in the Xuefengshan region have been compared with those of the same type of deposits in China and abroad. Then it is suggested that there is a significant potential for prospecting Ni,Co,Cu and Au ore deposit related to the mafic-ultramafic rocks in the Xuefengshan region,Hunan Province,especially the magmatic Ni-Co-Cu sulfide deposit and hydrothermal alteration type Au deposit.Furthermore,it is considered that there are good potentials for prospecting magmatic sulfide type Ni-Co-Cu deposits in Neoproterozoic mafic-ultramafic intrusions in the Tongdao-Hongjiang-Zhongfang-Guzhang belt,and the hydrothermal alteration type Au deposits in the Aikou magamatic belt and the Dahongshan area of the Aitouping-Dahongshan magamatic belt.
A certain progress for prospecting ore deposits related to mafic-ultramafic rocks in the Xuefengshan region has been made recently. Based on a large volume of field investigation,we have systematically summarized the geological and mineralization characteristics of the Changjie Ni ore deposit,the Zixi Au ore deposit,some Ni-Co-Cu-Au mineral occurrences,and the host mafic-ultramafic intrusions,in order to summarize metallogenic regulations and to guide further prospecting work in the area. Moreover,the metallogenic characteristics of Ni-Co-Cu-Au deposits in the Xuefengshan region have been compared with those of the same type of deposits in China and abroad. Then it is suggested that there is a significant potential for prospecting Ni,Co,Cu and Au ore deposit related to the mafic-ultramafic rocks in the Xuefengshan region,Hunan Province,especially the magmatic Ni-Co-Cu sulfide deposit and hydrothermal alteration type Au deposit.Furthermore,it is considered that there are good potentials for prospecting magmatic sulfide type Ni-Co-Cu deposits in Neoproterozoic mafic-ultramafic intrusions in the Tongdao-Hongjiang-Zhongfang-Guzhang belt,and the hydrothermal alteration type Au deposits in the Aikou magamatic belt and the Dahongshan area of the Aitouping-Dahongshan magamatic belt.
引文
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Li Z X,Li X H,Kinny P D,Wang J.1999.The breakup of Rodinia:Did it start with a mantle plume beneath South China?Earth and Planetary Science Letters,173(3):171-181
Li Z X,Zhang L H,Powell C M.1995.South China in Rodinia:Part of the missing link between Australia East Antarctica and Laurentia?Geology,23(5):407-410
Naldrett A J.1999.World-class Ni-Cu-PGE deposits:Key factors in their genesis.Mineralium Deposita,34(3):227-240
Qin K Z,Su B X,Sakyi P A,Tang D M,Li X H,Sun H,Xiao Q H,Liu PP.2011.SMS Zircon U-Pb Geochronology and Sr-Nd Isotopes of Ni-Cubearing mafic-ultramafic intrusions in Eastern Tianshan and Beishan in correlation with flood Basalts in Tarim Basin(NW China):Contraints on a Ca.280 Ma Mantle Plume.American Journal of Science,311(3):237-260
Schandl E S,Gorton M P.2012.Hydrothermal alteration and CO2metasomatism(natural carbon sequestration)of komatiites in the south-western Abitibi greenstone belt.Canadian Mineralogist,50(1):129-146
Schandl E S,Naldrett A J.1992.CO2metasomatism of serpentinites,south of Timmins,Ontario.Canadian Mineralogist,30(1):93-108
Wang J,Li Z X.2003.History of Neoproterozoic rift basins in South China:implications for Rodinia break-up.Precambrian Research,122(1-4):141-158
Wang X C,Li X H,Li W X,Li Z X.2007.Ca.825 Ma komatiitic basalts in South China:First evidence for>1500°C mantle melts by a Rodinian mantle plume.Geology,35(12):1103-1106
Wang X L,Zhou J C,Qiu J S,Gao J F.2004.Geochemistry of the Meso-to Neoproterozoic basic-acid rocks from Hunan Province,South China:Implications for the evolution of the western Jiangnan orogen.Precambrian Research,135(1-2):79-103
Wang X L,Zhou J C,Qiu J S,Jiang S Y,Shi Y R.2008.Geochronology and geochemistry of Neoproterozoic mafic rocks from western Hunan,South China:Implications for petrogenesis and post-orogenic extension.Geological Magazine,145(2):215-233
Wang X L,Zhou J C,Qiu J S,Zhang W L,Liu X M,Zhang G L.2006.LA-ICP-MS U-Pb zircon geochronology of the Neoproterozoic igneous rocks from Northern Guangxi,South China:Implications for tectonic evolution.Precambrian Research,145(1-2):111-130
Wu F Y,Wilde S A,Zhang G L,Sun D Y.2004.Geochronology and petrogenesis of the post-orogenic Cu-Ni sulfide-bearing mafic-ultramafic complexes in Jilin Province,NE China.Journal of Asian Earth Sciences,23(5):781-797
Zhang M J,Kamo S L,Li C S,Hu P Q,Ripley E M.2010.Precise U-Pb zircon-baddeleyite age of the Jinchuan sulfide ore-bearing ultramafic intrusion,western China.Mineralium Deposita,45(1):3-9
Zheng Y F,Wu R X,Wu Y B,Zhang S B,Yuan H L,Wu F Y.2008.Rift melting of juvenile arc-derived crust:Geochemical evidence from Neoproterozoic volcanic and granitic rocks in the Jiangnan Orogen,South China.Precambrian Research,163(3-4):351-383
Zhou J B,Li X H,Ge W C,Li Z X.2007.Age and origin of middle Neoproterozoic mafic magmatism in southern Yangtze Block and relevance to the break-up of Rodinia.Gondwana Research,12(1-2):184-197
Zhou M F,Arndt N T,Malpas J,Wang C Y,Kennedy A K.2008.Two magma series and associated ore deposit types in the Permian Emeishan large igneous province,SW China.Lithos,103(3-4):352-368
Zhou M F,Kennedy A K,Sun M,Malpas J,Lesher C M.2002.Neoproterozoic arc-related mafic intrusions along the Northern Margin of South China:Implications for the accretion of Rodinia.Journal of Geology,110(5):611-618
Zhou Y,Zhong H,Li C S,Ripley E W,Zhu W G,Bai Z J,Li C.2017.Geochronological and geochemical constraints on sulfide mineralization in the Qingmingshan mafic intrusion in the western part of the Proterozoic Jiangnan Orogenic Belt along the southern margin of the Yangtze Craton.Ore Geology Reviews,90:618-633
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