Reaction of subducted sediment with peridotite produces saline fluid inclusions in diamonds

Michael W. Foerster; Stephen F. Foley; Horst R. Marschall; Olivier Alard; Stephen Buhre; Anonymous

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Article de revue

Reaction of subducted sediment with peridotite produces saline fluid inclusions in diamonds

Michael W. Foerster, Stephen F. Foley, Horst R. Marschall, Olivier Alard, Stephen Buhre et Anonymous

V.M. Goldschmidt Conference - Program and Abstracts, Vol.29

Goldschmidt 2019

2019

Résumé

Asia

carbon dioxide

carbonates

chemical ratios

Commonwealth of Independent States

diamond

dunite

experimental studies

fluid inclusions

Geophysics of minerals and rocks

high pressure

Igneous and metamorphic petrology

igneous rocks

inclusions

kimberlite

laboratory studies

lithosphere

magnesite

mantle

marine sediments

melting

metamorphism

native elements

P-T conditions

peridotites

phase equilibria

plutonic rocks

potassium chloride

pressure

Russian Federation

salinity

sediments

sodium chloride

stability

Udachnaya Pipe

ultramafics

upper mantle

Yakutia Russian Federation

Indicateurs

1 Consultations de la notice

Détails

Titre: Reaction of subducted sediment with peridotite produces saline fluid inclusions in diamonds
Créateurs - sans rôle: Michael W. Foerster - Macquarie University, Department of Earth and Planetary Sciences Sydney AUS Australia
Stephen F. Foley
Horst R. Marschall
Olivier Alard
Stephen Buhre
Anonymous
Détails de publication: V.M. Goldschmidt Conference - Program and Abstracts, Vol.29
Colloque: Goldschmidt 2019
Éditeur: Goldschmidt Conference
Identifiants: 99136868909311
Unité académique: Géosciences Montpellier - GM
Langue: English
Type de ressource: Journal article