Magma flow directions of shallow dykes from the East Greenland volcanic margin inferred from magnetic fabric studies
Authors:
- J.-P CallotJCJ.-P Callot
- L GeoffroyLGL Geoffroy
- D MegeDMD Mege
- 1 July 2001
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 335 (3-4) , 313-329
Abstract
No abstract availableKeywords
This publication has 41 references indexed in Scilit:
- Post-breakup basaltic magmatism along the East Greenland Tertiary rifted marginEarth and Planetary Science Letters, 1998
- Volcanic Margin Concepts1995
- North Atlantic volcanic margins: Dimensions and production ratesJournal of Geophysical Research, 1994
- Large igneous provinces: Crustal structure, dimensions, and external consequencesReviews of Geophysics, 1994
- Evidence from magnetic fabric for the flow pattern of magma in the Mackenzie giant radiating dyke swarmNature, 1992
- Magmatic tectonic evolution of a volcanic rifted marginMarine Geology, 1991
- The E Greenland continental margin: a transition between oceanic and continental magmatismJournal of the Geological Society, 1982
- Un nouveau critere de sens de mise en place dans une caisse filonienne: Le “pincement” des mineraux aux epontesTectonophysics, 1979
- Flow and emplacement direction determined for selected basaltic bodies using magnetic susceptibility anisotropy measurementsEarth and Planetary Science Letters, 1978
- Hysteresis properties of titanomagnetites: Grain-size and compositional dependencePhysics of the Earth and Planetary Interiors, 1977