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The petrochemistry of jake_m: a martian mugearite

Science (New York, N.Y.) | 28 Sep 2013

EM Stolper, MB Baker, ME Newcombe, ME Schmidt, AH Treiman, A Cousin, MD Dyar, MR Fisk, R Gellert, PL King, L Leshin, S Maurice, SM McLennan, ME Minitti, G Perrett, S Rowland, V Sautter and RC Wiens
Abstract
“Jake_M,” the first rock analyzed by the Alpha Particle X-ray Spectrometer instrument on the Curiosity rover, differs substantially in chemical composition from other known martian igneous rocks: It is alkaline (>15% normative nepheline) and relatively fractionated. Jake_M is compositionally similar to terrestrial mugearites, a rock type typically found at ocean islands and continental rifts. By analogy with these comparable terrestrial rocks, Jake_M could have been produced by extensive fractional crystallization of a primary alkaline or transitional magma at elevated pressure, with or without elevated water contents. The discovery of Jake_M suggests that alkaline magmas may be more abundant on Mars than on Earth and that Curiosity could encounter even more fractionated alkaline rocks (for example, phonolites and trachytes).
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Concepts
Metamorphic rock, Lava, Mars, Rock, Petrology, Igneous rock, Granite, Magma
MeSH headings
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