Mesoscale pervasive felsic magma migration: alternatives to dyking
- 31 March 1999
- journal article
- Published by Elsevier BV in Lithos
- Vol. 46 (3), 393-410
- https://doi.org/10.1016/s0024-4937(98)00075-9
Abstract
No abstract availableThis publication has 40 references indexed in Scilit:
- Shear-zone systems and melts: feedback relations and self-organization in orogenic beltsJournal of Structural Geology, 1998
- Pervasive granitoid magma transfer through the lower–middle crust during non‐coaxial compressional deformationJournal of Metamorphic Geology, 1996
- The generation, segregation, ascent and emplacement of granite magma: the migmatite-to-crustally-derived granite connection in thickened orogensEarth-Science Reviews, 1994
- Mechanisms of continental growth in extensional arcs: An example from the Andean plate-boundary zoneGeology, 1994
- Granite magma generation, ascent and emplacement within a transpressional orogenJournal of the Geological Society, 1992
- Granitic magma transport by fracture propagationTectonophysics, 1992
- Why dikes?Geology, 1990
- Thermal control of basaltic fissure eruptionsNature, 1989
- Constraints on melting and magma production in the crustEarth and Planetary Science Letters, 1987
- High fluid pressures during regional metamorphism and deformation: Implications for mass transport and deformation mechanismsJournal of Geophysical Research, 1984