The origin of electrically conductive lower continental crust: saline water or graphite?
- 1 December 1993
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 81 (1-4) , 325-345
- https://doi.org/10.1016/0031-9201(93)90139-z
Abstract
No abstract availableKeywords
This publication has 84 references indexed in Scilit:
- Deep seismic reflection profiling and the growth of the continental crustPublished by Elsevier ,2003
- Electromagnetic images of modern and ancient subduction zonesTectonophysics, 1993
- Crustal structures from MT soundings in the Canadian CordilleraEarth and Planetary Science Letters, 1991
- Trapping of aqueous fluids in the deep crustGeophysical Research Letters, 1990
- Comparison of geoelectrical/tectonic models for suture zones in the western U.S.A. and eastern Europe: are black shales a possible source of high conductivities?Physics of the Earth and Planetary Interiors, 1989
- Source field problems in northern parts of the Baltic ShieldPhysics of the Earth and Planetary Interiors, 1989
- Carbon isotope compositions of fluid inclusions in charnockites from southern IndiaNature, 1988
- Magnetotelluric results opposing magma origin of crustal conductors in the rio grande riftTectonophysics, 1983
- Conductivity anomalies: lower crust or asthenosphere?Physics of the Earth and Planetary Interiors, 1981
- Heat flow and heat generation in the superior province of the canadian shieldTectonophysics, 1978