Infrastructural migmatitic upwelling in East Greenland interpreted as thermal convective structures
- 8 April 2003
- journal article
- Published by Elsevier
- Vol. 8 (1-2) , 77-93
- https://doi.org/10.1016/0301-9268(79)90039-1
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- Fold nappes as asymmetric mantled gneiss domes and ensialic orogenyPublished by Elsevier ,2003
- A horizontal tectonic regime in the Archaean of Greenland and its implications for early crustal thickeningPublished by Elsevier ,2003
- Thermal convection of water in a porous medium: Effects of temperature- and pressure-dependent thermodynamic and transport propertiesJournal of Geophysical Research, 1977
- The role of intercrustal convection in the formation of the structure of the continental crustTectonophysics, 1976
- Pre-Caledonian metamorphic complexes within the southern part of the East Greenland CaledonidesJournal of the Geological Society, 1976
- Review of Salt Tectonics in Relation to the Disposal of Radioactive Wastes in Salt FormationsGSA Bulletin, 1972
- Thermal convection below the solidus in a mantled gneiss dome, Fungwi Reserve, RhodesiaJournal of the Geological Society, 1971
- Magma convection, temperature distribution, and differentiationAmerican Journal of Science, 1969
- Oriented inclusions in granite; further evidence for floored magma chambersAmerican Journal of Science, 1969
- Comments on viscosity, crystal settling, and convection in granitic magmasAmerican Journal of Science, 1965