津巴布韦卢比(Ruby)矿床——南部非洲一典型的BIF型金矿床
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摘要
卢比金矿床位于津巴布韦克拉通中南部的马斯温戈绿岩带中,金矿体主要赋存在条带状含铁建造中的硫化物相、碳酸盐相中,成矿作用与火山喷发—沉积作用密切相关,为南部非洲一典型的BIF型金矿床。
The Ruby gold deposit is located at the Masvingo greenstone belt,south-central part of Zimbabwe craton. The ore bodies are mainly hosted in sulfide phase and carbonate phase of the banded iron formation,which are closely related to volcanic eruption and sedimental deposition process. The Ruby gold deposit is a typical BIF-hosted gold deposite in southern Africa.
The Ruby gold deposit is located at the Masvingo greenstone belt,south-central part of Zimbabwe craton. The ore bodies are mainly hosted in sulfide phase and carbonate phase of the banded iron formation,which are closely related to volcanic eruption and sedimental deposition process. The Ruby gold deposit is a typical BIF-hosted gold deposite in southern Africa.
引文
[1]沈保丰.太古宙绿岩带中金矿床的地质特征和找矿标志[J].国外前寒武纪地质,1987,(32):1-37.
[2]沈保丰,李上森,骆辉.前寒武纪条带状铁建造(BIF)中金的成矿作用[J].国外前寒武纪地质,1988,(1):1-34.
[3]J F Wilson.The Geology of the Country around Fort Victoria[M].Salisbury(Harare):Southern Rhodesia Geological Survey Bulletin,1964:1-245.
[4]J F Wilson.The Rhodesin Archaean craton-an essay in cratonic evolution[J].Philosophical Transactions of the Royal Society of London,1972,(273):389-411.
[5]Sharad Master,Andrey Bekker,Axel Hofmann.A review of the stratigraphy and geological setting of the Palaeoproterozoic Magondi Supergroup,Zimbabwe-Type locality for the Lomagundi carbon isotope excursion[J].Precambrian Research,2010,(182):254-273.
[6]V Markwitz,W D Maier,I.González-álvarez,T.C.Mc Cuaig,A.Porwal.Magmatic nickel sulfide mineralization in Zimbabwe:Review of deposits and development of exploration criteria for prospectivity analysis[J].Ore Geology Reviews,2010,(38):139-155.
[7]D S Bartholomew.Gold deposites of Zimbabwe[M].Harare:Zimbabwe Geological Survey,1990:1-75.
[8]楚旭春.非洲地质概况[M].北京:地图出版社,1982:1-54.
[9]G.A Gross.Tectonic systems and the deposition of iron-formation[J].Precambrian Res,1983,(30):63-80.
[10]J Veizer.Geologic evolution of the Archean-Early Proterozoic Earth[A].Princeton:Princeton University Press,1983,240-259.
[11]L A Derry,S B Jacobsen.The chemical evolution of Precambrian seawater:Evidence from REEs in banded iron formation[J].Geochim Cosmochim Acta,1990,(54):2965-2977.
[12]李碧乐,霍亮,李永胜.条带状铁建造(BIFs)研究的几个问题[J].矿物学报,2007,(2):205-210.
[13]周明宝.金矿成矿模式中若干问题的讨论[J].地质找矿论丛,1988,(3):70-75.
[14]刘静兰.前寒武纪条带状含铁建造中的金矿床—以东风山金矿床为例[J].地质学报,1987,(1):58-71.
[2]沈保丰,李上森,骆辉.前寒武纪条带状铁建造(BIF)中金的成矿作用[J].国外前寒武纪地质,1988,(1):1-34.
[3]J F Wilson.The Geology of the Country around Fort Victoria[M].Salisbury(Harare):Southern Rhodesia Geological Survey Bulletin,1964:1-245.
[4]J F Wilson.The Rhodesin Archaean craton-an essay in cratonic evolution[J].Philosophical Transactions of the Royal Society of London,1972,(273):389-411.
[5]Sharad Master,Andrey Bekker,Axel Hofmann.A review of the stratigraphy and geological setting of the Palaeoproterozoic Magondi Supergroup,Zimbabwe-Type locality for the Lomagundi carbon isotope excursion[J].Precambrian Research,2010,(182):254-273.
[6]V Markwitz,W D Maier,I.González-álvarez,T.C.Mc Cuaig,A.Porwal.Magmatic nickel sulfide mineralization in Zimbabwe:Review of deposits and development of exploration criteria for prospectivity analysis[J].Ore Geology Reviews,2010,(38):139-155.
[7]D S Bartholomew.Gold deposites of Zimbabwe[M].Harare:Zimbabwe Geological Survey,1990:1-75.
[8]楚旭春.非洲地质概况[M].北京:地图出版社,1982:1-54.
[9]G.A Gross.Tectonic systems and the deposition of iron-formation[J].Precambrian Res,1983,(30):63-80.
[10]J Veizer.Geologic evolution of the Archean-Early Proterozoic Earth[A].Princeton:Princeton University Press,1983,240-259.
[11]L A Derry,S B Jacobsen.The chemical evolution of Precambrian seawater:Evidence from REEs in banded iron formation[J].Geochim Cosmochim Acta,1990,(54):2965-2977.
[12]李碧乐,霍亮,李永胜.条带状铁建造(BIFs)研究的几个问题[J].矿物学报,2007,(2):205-210.
[13]周明宝.金矿成矿模式中若干问题的讨论[J].地质找矿论丛,1988,(3):70-75.
[14]刘静兰.前寒武纪条带状含铁建造中的金矿床—以东风山金矿床为例[J].地质学报,1987,(1):58-71.