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Volumn 142, Issue 6, 2002, Pages 714-723

The high-pressure stability of Mg-sursassite in a model hydrous peridotite: A possible mechanism for the deep subduction of significant volumes of H2O

Author keywords

[No Author keywords available]

Indexed keywords

HIGH PRESSURE; HYDROUS MINERAL; PERIDOTITE; STABILITY ANALYSIS; SUBDUCTION ZONE; SURSASSITE; ULTRAMAFIC ROCK;

EID: 0036127080     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-001-0318-5     Document Type: Article
Times cited : (36)

References (27)
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    • Phase transformations in serpentine at high pressures and temperatures and implications for subducting lithosphere
    • (1986) Phys Chem Mineral , vol.42 , pp. 252-262
    • Liu, L.-G.1
  • 11
    • 0024903085 scopus 로고
    • Stability fields of Mg-pumpellyite composition at high pressures and temperatures
    • (1989) Geophys Res Lett , vol.16 , pp. 847-849
    • Liu, L.-G.1
  • 18
    • 0023798493 scopus 로고
    • Experimental studies on metamorphism of crustal rocks under mantle pressures
    • (1988) Mineral Mag , vol.52 , pp. 1-26
    • Schreyer, W.1
  • 23
    • 0026286444 scopus 로고
    • Lubrication, gasketing and precision in multianvil experiments
    • (1991) Am Mineral , vol.76 , pp. 1092-1100
    • Walker, D.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.