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Theoretical analysis of the role of groundwater flow in the genesis of stratabound ore deposits; 1, Mathematical and numerical model

Garven, G., Freeze, R. A.·1984·American Journal of Science

Abstract

Carbonate-hosted lead-zinc deposits of the mississippi valley type are thought to have formed through the migration of warm (50 degrees -150 degrees C) subsurface fluids in sedimentary basins. The fundamental role of fluid flow is poorly understood; depending on the stage of evolution of a basin, either a compaction-drive or gravity-drive fluid-flow system may be developed. Quantitative examination of the role of one flow mechanism in ore genesis; gravity-driven groundwater flow. Equations governing fluid flow, heat transport, mass transport, and geochemical mass transfer. Numerical modeling techniques are used to develop a computer code for simulation of regional transport processes along cross sections. The finite-element method is applied to solve the steady-state, fluid-flow, and heat-transport equations, and a moving-particle random-walk algorithm is developed to predict the advection and dispersion of aqueous species.--Modified journal abstract.

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Metadata

Authors
Garven, G., & Freeze, R. A.
Venue
American Journal of Science
Published
1984-12-01
Volume
284
Issue
10
Pages
1085-1124
ISSN
0002-9599 (ISSN-L)
OpenAlex
W2108912216
Cited by
345
References
0
FWCI
13.76
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Theoretical analysis of the role of groundwater flow in the genesis of stratabound ore deposits; 1, Mathematical and numerical model. https://app.cochat.ai/papers/10.2475/ajs.284.10.1085
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Garven, G., & Freeze, R. A. (1984). Theoretical analysis of the role of groundwater flow in the genesis of stratabound ore deposits; 1, Mathematical and numerical model. American Journal of Science. https://doi.org/10.2475/ajs.284.10.1085

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