- Abstract:
-
The relative incompatibility of Ar and K are fundamental parameters in understanding the degassing history of the mantle. Clinopyroxene is the main host for K in most of the upper mantle, playing an important role in controlling the K/Ar ratio of residual mantle and the subsequent time-integrated evolution of 40Ar/36Ar ratios. Clinopyroxene also contributes to the bulk Ar partition coefficient that controls the Ar degassing rate during mantle melting. The partitioning of Ar and K between clin...
Expand abstract - Publication status:
- Published
- Publisher copy:
- 10.1016/S0016-7037(01)00784-0
-
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- Journal:
- GEOCHIMICA ET COSMOCHIMICA ACTA
- Volume:
- 66
- Issue:
- 3
- Pages:
- 507-519
- Publication date:
- 2002-02-05
- DOI:
- ISSN:
-
0016-7037
- URN:
-
uuid:0cd9db95-820d-44c5-b446-71af78bbcc7f
- Source identifiers:
-
163775
- Local pid:
- pubs:163775
- Language:
- English
- Copyright date:
- 2002
Journal article
Ar and K partitioning between clinopyroxene and silicate melt to 8 GPa
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