Lunar Gruithuisen and Mairan domes: Rheology and mode of emplacement

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Lunar Gruithuisen and Mairan domes: Rheology and mode of emplacement

[1] The lunar steep-sided Gruithuisen and Mairan domes are morphologically and spectrally distinctive structures and appear similar to terrestrial extrusive volcanic features characterized by viscous magma. We use the basic morphologic and morphometric characteristics of the domes to estimate the yield strengths ( 10 Pa), plastic viscosities ( 10 Pa s), and effusion rates ( 50 m/s) of the magma...

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Imbrian-age highland volcanism on the moon: the gruithuisen and mairan domes.

The Gruithuisen and Mairan domes on the moon represent morphologically and spectrally distinct nonmare extrusive volcanic features of Imbrian age. The composition, morphology, and age relationships of the domes indicate that nonmare extrusive volcanism in the northern Procellarum region of the moon continued until about 3.3 x 10(9) to 3.6 x 10(9) years ago and was partially contemporaneous with...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research: Planets

سال: 2003

ISSN: 0148-0227

DOI: 10.1029/2002je001909