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Longlou Rock Petrographic Characteristics and Division of Metallogenic Epoch and Stage of Mineralization of Funing in Yunnan

Ming Liu

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Abstract

Funing rock mass from the edge to the center is the high density of diabase phase,a fine-grained olive gabbro norite facies,the middle fine-grained gabbro norite facies the middle fine-grained hillock grain gabbro phase,the middle coarse-grained in the gang wen diorite phase.The native rock of copper and nickel ore deposit in the studied area is consisted of basic –ultrabasic magmatic rock,which has a good differentiation phenomenon.The silicate minerals in Nonglou copper nickel deposit are mainly olivine and pyroxene,a small amount of plagioclase and hornblende,very small amount of mica,calcite.The metal sulfides are pyrrhotite,pentlandite,chalcopyrite,magnetite,also contains a small amount of ilmenite and galena.Combined with ore mineral combination and output structure,orebody characteristics,ore deposit formation mainly experienced magmatic ore-forming period-structure-metamorphic hydrothermal mineralization period,and magmatic ore-forming period is divided into early magmatic liquation-crystallization differentiation stage-late magmatic metallogenic stages-ore pulp injection metallogenic stages-magmatic ore-forming period after hydrothermal metallogenic stages.The form of deposit experienced from magmatic liquation-crystallization differentiation stage to the late hydrothermal superimposed period.

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What this paper is about

Funing rock mass from the edge to the center is the high density of diabase phase,a fine-grained olive gabbro norite facies,the middle fine-grained gabbro norite facies the middle fine-grained hillock grain gabbro phase,the middle coarse-grained in the gang wen diorite phase.The native rock of copper and nickel ore deposit in the studied area is consisted of basic –ultrabasic magmatic rock,which has a good differentiation phenomenon.The silicate minerals in Nonglou copper nickel deposit are mainly olivine and pyroxene,a small amount of plagioclase and hornblende,very small amount of mica,calcite.The metal sulfides are pyrrhotite,pentlandite,chalcopyrite,magnetite,also contains a small amount of ilmenite and galena.Combined with ore mineral combination and output structure,orebody characteristics,ore deposit formation mainly experienced magmatic ore-forming period-structure-metamorphic hydrothermal mineralization period,and magmatic ore-forming period is divided into early magmatic liquation-crystallization differentiation stage-late magmatic metallogenic stages-ore pulp injection metallogenic stages-magmatic ore-forming period after hydrothermal metallogenic stages.The form of deposit experienced from magmatic liquation-crystallization differentiation stage to the late hydrothermal superimposed period.

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Available abstract

Funing rock mass from the edge to the center is the high density of diabase phase,a fine-grained olive gabbro norite facies,the middle fine-grained gabbro norite facies the middle fine-grained hillock grain gabbro phase,the middle coarse-grained in the gang wen diorite phase.The native rock of copper and nickel ore deposit in the studied area is consisted of basic –ultrabasic magmatic rock,which has a good differentiation phenomenon.The silicate minerals in Nonglou copper nickel deposit are mainly olivine and pyroxene,a small amount of plagioclase and hornblende,very small amount of mica,calcite.The metal sulfides are pyrrhotite,pentlandite,chalcopyrite,magnetite,also contains a small amount of ilmenite and galena.Combined with ore mineral combination and output structure,orebody characteristics,ore deposit formation mainly experienced magmatic ore-forming period-structure-metamorphic hydrothermal mineralization period,and magmatic ore-forming period is divided into early magmatic liquation-crystallization differentiation stage-late magmatic metallogenic stages-ore pulp injection metallogenic stages-magmatic ore-forming period after hydrothermal metallogenic stages.The form of deposit experienced from magmatic liquation-crystallization differentiation stage to the late hydrothermal superimposed period.

Key concepts: Geology, Geochemistry, Gabbro, Porphyritic, Diorite, Pyroxene, Olivine, Zircon

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Longlou Rock Petrographic Characteristics and Division of Metallogenic Epoch and Stage of Mineralization of Funing in Yunnan — Research Paper | ScholarLens