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An empirical modification of Dodson's equation for closure temperature in binary systems

โœ Scribed by Karin Ehlers; Roger Powell


Book ID
118887020
Publisher
Elsevier Science
Year
1994
Tongue
English
Weight
795 KB
Volume
58
Category
Article
ISSN
0016-7037

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Continuing element exchange between minerals during cooling from the metamorphic peak modifies mineral compositions from those existing at the peak. After closure, when the minerals stop changing composition, the compositional relationships hold important information regarding, for example, cooling