Helium isotopic ratios in fluid inclusions from fluorite-rich Mississippi Valley-Type district of Asturias, northern Spain
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- SÁNCHEZ VIRGINIA
- Dept. Cristalografía y Mineralogía, Facultad de Ciencias Geológicas, Universidad Complutense
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- STUART FINLAY M.
- Isotope Geosciences Unit, SUERC
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- MARTÍN-CRESPO TOMÁS
- ESCET, E. Departamental II, Universidad Rey Juan Carlos
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- VINDEL ELENA
- Dept. Cristalografía y Mineralogía, Facultad de Ciencias Geológicas, Universidad Complutense
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- CORBELLA MERCÉ
- Dept. Geología, Facultat de Ciences, Universitat Autònoma
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- CARDELLACH ESTEVE
- Dept. Geología, Facultat de Ciences, Universitat Autònoma
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Abstract
Helium isotopes have been measured in fluorite and sulphides from fluorite-rich Mississippi Valley-type (MVT) deposits from Asturias, Spain, in order to assess the involvement of mantle and crust-derived volatiles in the genesis of the deposits. The 3He/4He of the ore fluids are ≤0.1 Ra ruling out a contribution of mantle-derived magmatic helium in the inclusion fluids. Data support a crustal source for the volatiles and is consistent with the existing basinal model for the genesis of the Asturias MVT mineralization by mixing of sedimentary brines with infiltrating superficial fluids.
Journal
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- GEOCHEMICAL JOURNAL
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GEOCHEMICAL JOURNAL 44 (1), e1-e4, 2010
GEOCHEMICAL SOCIETY OF JAPAN
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Details 詳細情報について
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- CRID
- 1390282679529608832
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- NII Article ID
- 10027720258
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- NII Book ID
- AA00654975
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- COI
- 1:CAS:528:DC%2BC3cXltFWlt7o%3D
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- ISSN
- 18805973
- 00167002
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- NDL BIB ID
- 10936415
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- Text Lang
- en
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed