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- W2363103626 abstract "According to the analysis of structural deformation,ore-bearing characteristics,metallogenetic rule and ore-controlling factor of the Lukuishan syncline and the geological geophysical comprehensive ore-prospecting work on the east limb,the siderite ore-origin bed in Dalongkou Formation of Kunyang Group in the Lukuishan rift experienced many times of interbed dislocation or crushing after the structural deformation and metamorphism,The original sedimentary and metamorphie siderite ore-origin bed or poor orebody was changed by the later secondary leaching concentration,ore-bearing hydrothermal alteration and interbed slipping structure and then formed the stratiform rich iron orebody similar to the original sedimentation and with hydrothermal alteration,tectonite characteristics.According to the pitting exploration,the secondary enrichment ore deposits distributed discontinuously on the east and west limbs of Lukuishan syncline are actually the epigenetic sedimentary metamorphic ore deposits controlled by the ring fault zone with interbed structure characteristics.And the hydrothermal metasomatic and filling veinlike orebodies formed by the surface and shallow brittle faults superimposed partly on the stratiformorebodies in the ring fault zone,which increases the possibility of discovering the thick nest orebodies.These new metallogenetic and ore-controlloing rules provide a practical basis for the re-avaluation of Lukuishan-type sedimentary metamorphic iron depositand point out a new ore-prospecting direction in this area." @default.
- W2363103626 created "2016-06-24" @default.
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- W2363103626 date "2004-01-01" @default.
- W2363103626 modified "2023-09-23" @default.
- W2363103626 title "THE RELATIONSHIP BETWEEN NAPPE SYSTEM AND METALLOGENESIS OF THE LUKUISHAN IRON DEPOSIT" @default.
- W2363103626 hasPublicationYear "2004" @default.
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