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KARST CAVE DEVELOPMENT AND MINERAL DEPOSIT FEATURES IN HUNAN BOUNDARY

Changmin Chen

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Abstract

This paper describes diwa karst cave evolution along the Hunan boundary.Differences in geotectonics develop disequilibrium effects in the karst cave of diwa regions,Such effects upon cave development are changed in underground currents which influence the shape of caves. the type of cave, its spatial and temporal evolution and can completely remake caves in diwa areas. The products of such changes affect the cave mineral deposit features, cave metallogenetic mechanisms. Therefore, the type of cave deposits and evolution are law of cave mineral deposits in diwa areas.

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What this paper is about

This paper describes diwa karst cave evolution along the Hunan boundary.Differences in geotectonics develop disequilibrium effects in the karst cave of diwa regions,Such effects upon cave development are changed in underground currents which influence the shape of caves. the type of cave, its spatial and temporal evolution and can completely remake caves in diwa areas. The products of such changes affect the cave mineral deposit features, cave metallogenetic mechanisms. Therefore, the type of cave deposits and evolution are law of cave mineral deposits in diwa areas.

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Available abstract

This paper describes diwa karst cave evolution along the Hunan boundary.Differences in geotectonics develop disequilibrium effects in the karst cave of diwa regions,Such effects upon cave development are changed in underground currents which influence the shape of caves. the type of cave, its spatial and temporal evolution and can completely remake caves in diwa areas. The products of such changes affect the cave mineral deposit features, cave metallogenetic mechanisms. Therefore, the type of cave deposits and evolution are law of cave mineral deposits in diwa areas.

Key concepts: Cave, Karst, Geology, Mineral, Disequilibrium, Geochemistry, Archaeology, Paleontology

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