In-situ X-ray diffraction of aragonite and dolomite at high pressure and high temperature. Evidence for dolomite breakdown to aragonite and magnesite | INSTITUT DE PHYSIQUE DU GLOBE DE PARIS

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  In-situ X-ray diffraction of aragonite and dolomite at high pressure and high temperature. Evidence for dolomite breakdown to aragonite and magnesite

Type de publication:

Journal Article

Source:

Am. mineral., Volume 81, p.611-624. (1996)

ISBN:

0003-004X

Numéro d'appel:

PUB

URL:

http://ammin.minsocam.org

Mots-clés:

Géochimie des isotopes stables, UPRESA 7047

Notes:

(The) American mineralogist