(2) H/(1) H measurements of amphiboles and nominally anhydrous minerals (clinopyroxene, garnet and diamond) using high-temperature continuous flow elemental analyser/pyrolysis/isotope ratio mass spectrometry.
Identifieur interne : 001356 ( Main/Exploration ); précédent : 001355; suivant : 001357(2) H/(1) H measurements of amphiboles and nominally anhydrous minerals (clinopyroxene, garnet and diamond) using high-temperature continuous flow elemental analyser/pyrolysis/isotope ratio mass spectrometry.
Auteurs : François Fourel [France] ; Christophe Lécuyer [France] ; Attila Demeny [Hongrie] ; Philippe Boulvais [France] ; Lutz Lange [Allemagne] ; Dorrit E. Jacob [Australie] ; Istvan Kovacs [Hongrie]Source :
- Rapid communications in mass spectrometry : RCM [ 1097-0231 ] ; 2017.
Abstract
We have used a high-precision, high-efficiency method for the measurement of the (2) H/(1) H ratios of hydrous silicates (amphiboles) and nominally anhydrous minerals (NAM) such as clinopyroxene, garnet and diamond, which are usually extremely resistant to pyrolysis. This opens up new fields of investigation to better understand the conditions of formation for deep-Earth minerals.
DOI: 10.1002/rcm.7996
PubMed: 28940398
Affiliations:
- Allemagne, Australie, France, Hongrie
- Auvergne-Rhône-Alpes, Rhône-Alpes, Région Bretagne
- Lyon, Rennes, Villeurbanne
- Université Claude Bernard Lyon 1, Université de Rennes 1
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Le document en format XML
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<front><div type="abstract" xml:lang="en">We have used a high-precision, high-efficiency method for the measurement of the (2) H/(1) H ratios of hydrous silicates (amphiboles) and nominally anhydrous minerals (NAM) such as clinopyroxene, garnet and diamond, which are usually extremely resistant to pyrolysis. This opens up new fields of investigation to better understand the conditions of formation for deep-Earth minerals.</div>
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