Interactions between organic compounds and olivine under aqueous conditions: A potential role for organic distribution in carbonaceous chondrites

Olivine is a principal anhydrous silicate mineral in chondritic meteorites. The structure of this mineral is composed of independent SiO4 tetrahedra linked by divalent cations (mainly Mg). Under hydrothermal conditions, olivine is transformed into serpentine, which is a major hydrated phyllosilicate...

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Bibliographic Details
Published in:	Meteoritics & planetary science Vol. 56; no. 2; pp. 195 - 205
Main Authors:	Muneishi, Keisuke, Naraoka, Hiroshi
Format:	Journal Article
Language:	English
Published:	Hoboken Wiley Subscription Services, Inc 01-02-2021
Subjects:	Adsorption Asteroids Carbonaceous chondrites Cations Chondrites Chromatography Cyclic compounds Divalent cations Fluid dynamics Fluid flow Liquid chromatography Low temperature Meteorites Meteors & meteorites Olivine Organic compounds Organic matter Serpentine Solid phases Tetrahedra
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