Coronae formation on Venus via extension and lithospheric instability-Reference-Cited by-同舟云学术

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Coronae formation on Venus via extension and lithospheric instability

Published:2014-12 Issue:12 Volume:119 Page:2568-2582
ISSN:2169-9097
Container-title:Journal of Geophysical Research: Planets
language:en
Short-container-title:J. Geophys. Res. Planets

Author:

Piskorz Danielle¹,Elkins-Tanton Linda T.²,Smrekar Suzanne E.³

Affiliation:

1. Division of Geological and Planetary Sciences; California Institute of Technology; Pasadena California USA

2. School of Earth and Space Exploration; Arizona State University; Tempe Arizona USA

3. Jet Propulsion Laboratory; California Institute of Technology; Pasadena California USA

Funder

National Science Foundation

National Aeronautics and Space Administration

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014JE004636/fullpdf

Reference61 articles.

1. Simulating the thermochemical magmatic and tectonic evolution of Venus's mantle and lithosphere: Two-dimensional models;Armann;J. Geophys. Res.,2012

2. The geology and geomorphology of the venus surface as revealed by the radar images obtained by veneras 15 and 16;Barsukov, V. L.;J. Geophys. Res.,1986

3. Evolution of LILE-enriched small melt fractions in the lithospheric mantle: A case study from the East African Rift;Bedini;Earth Planet. Sci. Lett.,1997

4. Convective instability of thickening mantle lithosphere;Conrad;Geophys. J. Int.,2000

5. Rates of magma emplacements and volcanic output;Crisp;J. Volcanol. Geotherm. Res.,1984

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