Mercury's Caloris basin: Continuity between the interior and exterior plains
Author:
Affiliation:
1. School of Physical Sciences; Open University; Milton Keynes UK
2. Dipartimento di Fisica e Geologia; Università degli Studi di Perugia; Perugia Italy
3. Istituto di Astrofisica e Planetologia Spaziali; INAF; Rome Italy
Funder
UK Space Agency and the Science and Technology Funding Council
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/10.1002/2017JE005282/fullpdf
Reference43 articles.
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3. Mercury's global contraction much greater than earlier estimates;Byrne;Nat. Geosci.,2014
4. Widespread effusive volcanism on Mercury likely ended by about 3.6 Ga;Byrne;Geophys. Res. Lett.,2016
5. A laboratory model of surface crust formation and disruption on lava flows through non-uniform channels;Cashman;Bull. Volcanol.,2006
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