Constraints on the deep thermal structure of the Dharwar craton, India, from heat flow, shear wave velocities, and mantle xenoliths

Author:

Roy Sukanta,Mareschal Jean-Claude

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference104 articles.

1. Heat production in an Archean crustal profile and implications for heat flow and mobilization of heat producing elements;Ashwal;Earth Planet. Sci. Lett.,1987

2. S velocity variations beneath North America;Bedle;J. Geophys. Res.,2009

3. The crust-mantle structure of the Indian Peninsula from surface wave dispersion;Bhattacharya;Geophys. J. R. Astron. Soc.,1974

4. Observation and inversion of surface wave group velocities across central India;Bhattacharya;Bull. Seismol. Soc. Am.,1981

5. Tectonic framework and evolution of graben basins of India;Biswas,1993

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