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Volumn 184, Issue 2, 2001, Pages 529-534

Experimental investigation on dolomite dissociation into aragonite+magnesite up to 8.5 GPa

Author keywords

Argonite; Dissociation; Dolomite; Magnesite; P T conditions

Indexed keywords

ARAGONITE; DOLOMITE; HIGH PRESSURE; HIGH TEMPERATURE; MAGNESITE; METAMORPHISM; P-T CONDITIONS;

EID: 0035112138     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0012-821X(00)00346-0     Document Type: Article
Times cited : (90)

References (27)
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    • Zhang, R.Y.1    Liou, J.G.2
  • 9
    • 0030454752 scopus 로고    scopus 로고
    • In situ X-ray diffraction of aragonite and dolomite at high pressure and high temperature: Evidence for dolomite breakdown to aragonite and magnesite
    • (1996) Am. Miner , vol.81 , pp. 611-624
    • Martinez, I.1    Zhang, J.2    Reeder, R.J.3
  • 16
    • 0027423848 scopus 로고
    • Petrology of a diamond and coesite-bearing metamorphic terrane: Dabie Shan, China
    • (1993) Eur. J. Miner , vol.5 , pp. 659-675
    • Okay, A.I.1
  • 25
    • 0026498139 scopus 로고
    • Coesite-bearing eclogites from the Dabie Mountains, central China: Petrogenesis, P-T paths, and implications for regional tectonics
    • (1992) J. Geol , vol.100 , pp. 231-250
    • Wang, X.1    Liou, J.G.2    Maruyama, S.3


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.