The influence of poorly interconnected fault zone flow paths on spring geochemistry
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چکیده
منابع مشابه
The influence of poorly interconnected fault zone flow paths on spring geochemistry
Thermal springs commonly occur along faults because of the enhanced vertical permeability afforded by fracture zones. Field and laboratory studies of fault zone materials document substantial heterogeneities in fracture permeabilities. Modeling and field studies of springs suggest that spatial variations in permeability strongly influence spring locations, discharge rates and temperatures. The ...
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ژورنال
عنوان ژورنال: Geofluids
سال: 2008
ISSN: 1468-8115,1468-8123
DOI: 10.1111/j.1468-8123.2008.00208.x