Theoretical analysis of the role of groundwater flow in the genesis of stratabound ore deposits; 2, Quantitative results

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ID: 292804
1984
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Abstract
Sensitivity analysis indicate that gravity-driven groundwater flow systems are capable of sustaining favorable fluid-flow rates, temperatures, and metal concentrations for ore formation at groundwater-discharge areas near the edge of a basin. Under a gravity-drive mechanism, groundwater flows from recharge areas in the elevated regions of a foreland basin to discharge areas in lower-elevation regions. Flow patterns and rates are largely dependent on the basin geometry, the water-table configuration, and the subsurface variation in permeability.\--Modified journal abstract.
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openalex_W2320215452 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Grant Garven, R A Freeze
Journal american journal of science
Year 1984
DOI
10.2475/ajs.284.10.1125
URL
https://ajsonline.org/article/60300.pdf
Keywords Keywords not found

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