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Volumn 65, Issue 21, 2001, Pages 4043-4065

Hydrous phase equilibria of a Mexican high-silica andesite: A candidate for a mantle origin?

Author keywords

[No Author keywords available]

Indexed keywords

ANDESITE; GEOCHEMISTRY; LAVA FLOW; MANTLE SOURCE; PHASE EQUILIBRIUM; PHENOCRYST;

EID: 0035201620     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0016-7037(01)00708-6     Document Type: Article
Times cited : (105)

References (34)
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    • (1995) Contrib. Mineral. Petrol , vol.119 , pp. 197-212
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    • Luhr, J.F.1
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    • Shape of the subducted Rivera and Cocos plates in Southern Mexico: Seismic and tectonic implications
    • (1995) J. Geophys. Res , vol.100 , Issue.7 B , pp. 12357-12373
    • Pardo, M.1    Suarez, G.2
  • 28
    • 0028192665 scopus 로고
    • Thermodynamic data from redox reactions at high temperatures III, Activity-composition relations in Ni-Pd alloys from EMF measurements at 850-1250 K, and calibration of the NiO + Ni-Pd assemblage as a redox sensor
    • (1994) Contrib. Mineral. Petrol , vol.116 , pp. 327-339
    • Pownceby, M.I.1    O'Neill, H.S.C.2
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    • Viscosities of magmatic silicate liquids: An empirical method of prediction
    • (1972) Am. J. Sci , vol.272 , pp. 870-893
    • Shaw, H.R.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.