subject predicate object context
33569 Creator 33d05223e7b4d60c57d022f20621f60f
33569 Creator 96fdb8f74aad60e762b1aef18d80ab45
33569 Creator b75227dc49245aab76a534b836099ab7
33569 Creator d8b3b90e24f10b122cfbd5afecaaa40e
33569 Creator 480f5038acb8373736276bd8797a1fc9
33569 Creator 81bdad45ff4dac76717374f49f37ccdf
33569 Creator ext-5c34853686ba6a225ce5fa3d7106846e
33569 Creator f408be3371e41faa3267614d74064a12
33569 Date 2011
33569 Is Part Of repository
33569 abstract The nakhlite meteorites, widely accepted to originate on Mars, preserve complex mixtures of silicate alteration, carbonates, sulphates, halides, oxides and iron oxyhydroxides. These phases may have formed at different times, under different fluid flow regimes (groundwater, hydrothermal, crater lake), experiencing a range of water-rock ratios, evaporative histories, and varying degrees of interaction with the atmosphere and bedrock. Using information gathered from our 3D investigations of Nakhla’s fluid pathways we have undertaken a range of insitu geochemical and isotopic analyses of carbonate, sulphate and halite in the Nakhla meteorite.
33569 authorList authors
33569 presentedAt ext-b70af2161a5f6ee32b2ad1b451469793
33569 status peerReviewed
33569 type AcademicArticle
33569 type Article
33569 label Needham, A. W. ; Starkey, N. A. ; Johnson, D. ; Tomkinson, T. ; Guillermier, C. ; Abel, R. L.; Franchi, I. A. and Grady, M. M. (2011). Origin and composition of carbonates, sulphates and halite on Mars. In: 74th Annual Meeting of the Meteoritical Society, 8-12 Aug 2011, London, UK.
33569 label Needham, A. W. ; Starkey, N. A. ; Johnson, D. ; Tomkinson, T. ; Guillermier, C. ; Abel, R. L.; Franchi, I. A. and Grady, M. M. (2011). Origin and composition of carbonates, sulphates and halite on Mars. In: 74th Annual Meeting of the Meteoritical Society, 8-12 Aug 2011, London, UK.
33569 Title Origin and composition of carbonates, sulphates and halite on Mars
33569 in dataset oro