The role of groundwater flow in the genesis of stratabound ore deposits: a quantitative analysis
Many conceptual models have been proposed to explain the fluid-flow mechanism responsible for the origin of carbonate-hosted lead-zinc deposits such as those in the Mississippi Valley and at Pine Point. This study is devoted to the quantitative investigation of one ore-genesis mechanism gravity-dr...
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| Language: | en_US |
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The University of Arizona.
1982
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| Online Access: | http://hdl.handle.net/10150/626805 http://arizona.openrepository.com/arizona/handle/10150/626805 |