Volcanism on mercury: Evidence from the first MESSENGER flyby

James W. Head, Scott L. Murchie, Louise M. Prockter, Mark Robinson, Sean C. Solomon, Robert G. Strom, Clark R. Chapman, Thomas R. Watters, William E. McClintock, David T. Blewett, Jeffrey J. Gillis-Davis

Research output: Contribution to journalArticle

131 Scopus citations

Abstract

The origin of plains on Mercury, whether by volcanic flooding or impact ejecta ponding, has been controversial since the Mariner 10 flybys (1974-75). High-resolution images (down to 150 meters per pixel) obtained during the first MESSENGER flyby show evidence for volcanic vents around the Caloris basin inner margin and demonstrate that plains were emplaced sequentially inside and adjacent to numerous large impact craters, to thicknesses in excess of several kilometers. Radial graben and a floor-fractured crater may indicate intrusive activity. These observations, coupled with additional evidence from color images and impact crater size-frequency distributions, support a volcanic origin for several regions of plains and substantiate the important role of volcanism in the geological history of Mercury.

Original languageEnglish (US)
Pages (from-to)69-72
Number of pages4
JournalScience
Volume321
Issue number5885
DOIs
StatePublished - Jul 4 2008

ASJC Scopus subject areas

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    Head, J. W., Murchie, S. L., Prockter, L. M., Robinson, M., Solomon, S. C., Strom, R. G., Chapman, C. R., Watters, T. R., McClintock, W. E., Blewett, D. T., & Gillis-Davis, J. J. (2008). Volcanism on mercury: Evidence from the first MESSENGER flyby. Science, 321(5885), 69-72. https://doi.org/10.1126/science.1159256