Journal article
Numerical models, geochemistry and the zero-paradox noble-gas mantle.
- Abstract:
-
Numerical models of whole-mantle convection demonstrate that degassing of the mantle is an inefficient process, resulting in ca. 50% of the (40)Ar being degassed from the mantle system. In this sense the numerical simulations are consistent with the (40)Ar mass balance between the atmosphere and mantle reservoir. These models, however, are unable to preserve the large-scale heterogeneity predicted by models invoking geochemical layering of the mantle system. We show that the three most import...
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- Publication status:
- Published
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- Publisher copy:
- 10.1098/rsta.2002.1083
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Authors
Bibliographic Details
- Journal:
- Philosophical transactions. Series A, Mathematical, physical, and engineering sciences
- Volume:
- 360
- Issue:
- 1800
- Pages:
- 2611-2631
- Publication date:
- 2002-11-01
- DOI:
- EISSN:
-
1471-2962
- ISSN:
-
1364-503X
- Source identifiers:
-
82195
Item Description
- Language:
- English
- Keywords:
- Pubs id:
-
pubs:82195
- UUID:
-
uuid:b5f12df6-9410-446b-8688-9081b219a3ba
- Local pid:
- pubs:82195
- Deposit date:
- 2012-12-19
Terms of use
- Copyright date:
- 2002
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