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Duckworth, Owen W, Martin, Scot T (2004) Role of molecular oxygen in the dissolution of siderite and rhodochrosite. Geochimica et Cosmochimica Acta, 68 (3) 607-621 doi:10.1016/s0016-7037(03)00464-2

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Reference TypeJournal (article/letter/editorial)
TitleRole of molecular oxygen in the dissolution of siderite and rhodochrosite
JournalGeochimica et Cosmochimica Acta
AuthorsDuckworth, Owen WAuthor
Martin, Scot TAuthor
Year2004 (February)Volume68
Issue3
PublisherElsevier BV
DOIdoi:10.1016/s0016-7037(03)00464-2Search in ResearchGate
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Mindat Ref. ID349459Long-form Identifiermindat:1:5:349459:6
GUID0
Full ReferenceDuckworth, Owen W, Martin, Scot T (2004) Role of molecular oxygen in the dissolution of siderite and rhodochrosite. Geochimica et Cosmochimica Acta, 68 (3) 607-621 doi:10.1016/s0016-7037(03)00464-2
Plain TextDuckworth, Owen W, Martin, Scot T (2004) Role of molecular oxygen in the dissolution of siderite and rhodochrosite. Geochimica et Cosmochimica Acta, 68 (3) 607-621 doi:10.1016/s0016-7037(03)00464-2
In(2004, February) Geochimica et Cosmochimica Acta Vol. 68 (3) Elsevier BV

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Duckworth, Owen W, Martin, Scot T (2003) Connections between surface complexation and geometric models of mineral dissolution investigated for rhodochrosite. Geochimica et Cosmochimica Acta, 67 (10) 1787-1801 doi:10.1016/s0016-7037(02)01305-4
Duckworth, Owen W, Martin, Scot T (2001) Surface complexation and dissolution of hematite by C 1 -C 6 dicarboxylic acids at pH = 5.0. Geochimica et Cosmochimica Acta, 65 (23) 4289-4301 doi:10.1016/s0016-7037(01)00696-2
Tang, Yuanzhi, Martin, Scot T. (2011) Siderite dissolution in the presence of chromate. Geochimica et Cosmochimica Acta, 75 (17) 4951-4962 doi:10.1016/j.gca.2011.06.024
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