The “Panvel Flexure” along the Western Indian continental margin: an extensional fault structure related to Deccan magmatism
- 1 January 1995
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 241 (1-2) , 165-178
- https://doi.org/10.1016/0040-1951(94)00077-m
Abstract
No abstract availableKeywords
This publication has 46 references indexed in Scilit:
- Implications of mantle plume structure for the evolution of flood basaltsEarth and Planetary Science Letters, 1990
- Deccan flood basalts and the Cretaceous/Tertiary boundaryNature, 1988
- The Cretaceous‐Tertiary boundary events: External or internal causes?Eos, 1987
- Stratigraphy, composition and form of the Deccan Basalts, Western Ghats, IndiaBulletin of Volcanology, 1986
- On utility of space-borne vector magnetic measurements in crustal studiesPhysics of the Earth and Planetary Interiors, 1986
- Structure and evolution of the western continental margin of India deduced from gravity, seismic, geomagnetic and geochronological studiesPhysics of the Earth and Planetary Interiors, 1985
- Plate movement and continental magmatismNature, 1974
- Plume-Generated Triple Junctions: Key Indicators in Applying Plate Tectonics to Old RocksThe Journal of Geology, 1973
- New Data on Afar TectonicsNature Physical Science, 1972
- Deccan basaltsLithos, 1972