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Volumn 21, Issue 2, 1994, Pages 145-148

The transition from porous to channelized flow due to melt/rock reaction during melt migration

Author keywords

[No Author keywords available]

Indexed keywords

CHANNELIZED FLOW; MELT MIGRATION; MELT/ROCK REACTION; OLIVINE; POROUS FLOW; PYROXENE;

EID: 0028193394     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1029/93GL03052     Document Type: Article
Times cited : (119)

References (17)
  • 7
    • 0025262874 scopus 로고
    • Reaction between ultramafic wall rock and fractionating basaltic magma, Part I: Phase relations, the origin of calc‐alkaline magma series, and formation of discordant dunite
    • (1990) Journal of Petrology , vol.31 , pp. 51-98
    • Keleman, P.B.1
  • 9
    • 84986392999 scopus 로고
    • Structure, rheology, and permeability of partially molten rocks at low melt fractions, American Geophysical Union, Washington, D.C
    • (1992) Mantle Flow Morgan , pp. 103-121
    • Kohlstedt, D.L.1
  • 10
    • 84984434209 scopus 로고
    • Pacific lower crustal and shallow mantle sections recovered
    • (1993) Eos Trans. AGU , vol.74 , pp. 297
  • 12
  • 17
    • 0027063140 scopus 로고
    • Evidence for melt segregation towards fractures in the Horoman mantle peridotite complex
    • (1992) Nature , vol.359 , pp. 52-55
    • Takahashi, N.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.