Authors
John M Ferry, Gregory M Dipple
Publication date
1991/3/1
Journal
Geology
Volume
19
Issue
3
Pages
211-214
Publisher
Geological Society of America
Description
A general model that relates fluid flow along a temperature gradient to chemical reaction in rocks can be used to quantitatively interpret petrologic and geochemical data on metasomatism from ancient flow systems in terms of flow direction and time-integrated fluid flux. The model is applied to regional metamorphism, quartz veins, and a metasomatized ductile fault zone.
Total citations
Scholar articles
JM Ferry, GM Dipple - Geology, 1991