The scale-invariant nature of migmatite from the Oberpfalz, NE Bavaria and its significance for melt transport

Tectonophysics

Volumn 302, Issue 3-4, 1999, Pages 297-305

  Tanner, David C ^a,b  

^a UNIVERSITY OF FREIBURG   (Germany)

^b UNIVERSITY OF GÖTTINGEN   (Germany)

Author keywords

Fractals; Granite; Melt; Migmatite

Indexed keywords

EID: 0000866727     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0040-1951(98)00286-8     Document Type: Article

References (13)

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9. Hirata, T., 1989. The fractal geometry of flow paths in the natural fractures in rock and the approach to percolation. In: Scholz, C.H.M. (Ed.), Fractals in Geophysics. Birkhäuser, Basel, Boston, Berlin, pp. 158-170.
10. Jaeger, J.C., Cook, N.G.W., 1979. Fundamentals of Rock Mechanics. Chapman and Hall, London, 593 pp.
11. Jurewicz, S., Watson, E., 1985. The distribution of partial melt in a granitic system: the application of liquid phase sintering theory. Geochim. Cosmochim. Acta 49, 1109-1121.
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13. Laporte, D., Watson, E.B., 1995. Experimental and theoretical constraints on melt distribution in crustal sources: The effect of crystalline anisotropy on melt interconnectivity. Chem. Geol. 124, 161-184.