Sources of in-situ 36Cl in basaltic rocks. Implications for calibration of production rates

I. Schimmelpfennig; L. Benedetti; R. Finkel; R. Pik; P.-H. Blard; D. Bourles; P. Burnard; A. Williams

doi:10.1016/j.quageo.2009.06.003

Journal articles

Sources of in-situ 36Cl in basaltic rocks. Implications for calibration of production rates

I. Schimmelpfennig L. Benedetti ¹ R. Finkel ^{1, 2} R. Pik ³ P.-H. Blard ^{4, 3} D. Bourles ¹ P. Burnard ³ A. Williams ⁵

1 CEREGE - Centre européen de recherche et d'enseignement des géosciences de l'environnement

2 EPS - Department of Earth and Planetary Science [UC Berkeley]

3 CRPG - Centre de Recherches Pétrographiques et Géochimiques

4 Division of Geological and Planetary Sciences [Pasadena]

5 MOHC - Met Office Hadley Centre

Abstract : no abstract

Document type :

Journal articles

Domain :

Sciences of the Universe [physics]

Sciences of the Universe [physics] / Continental interfaces, environment

Sciences of the Universe [physics] / Earth Sciences

Sciences of the Universe [physics] / Earth Sciences / Geomorphology

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https://hal-amu.archives-ouvertes.fr/hal-01458885
Contributor : Régis Braucher <>
Submitted on : Tuesday, February 7, 2017 - 9:36:52 AM
Last modification on : Saturday, October 3, 2020 - 3:17:12 AM

Sources of in-situ 36Cl in basaltic rocks. Implications for calibration of production rates

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Sources of in-situ 36Cl in basaltic rocks. Implications for calibration of production rates

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