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Archaean asteroid impacts, banded iron formations and MIF-S anomalies: A discussion

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Glikson, Andrew

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The origin of mass-independent fractionation (MIF-S) of sulphur isotopes (δ33S) recorded in sediments older than 2.45 Ga is widely interpreted in terms of UV-triggered reactions under oxygen-poor ozone-depleted atmosphere conditions (Farquhar, J., Bao, H

dc.contributor.authorGlikson, Andrew
dc.date.accessioned2015-12-08T22:19:20Z
dc.identifier.issn0019-1035
dc.identifier.urihttp://hdl.handle.net/1885/31528
dc.description.abstractThe origin of mass-independent fractionation (MIF-S) of sulphur isotopes (δ33S) recorded in sediments older than 2.45 Ga is widely interpreted in terms of UV-triggered reactions under oxygen-poor ozone-depleted atmosphere conditions (Farquhar, J., Bao, H
dc.publisherAcademic Press
dc.sourceIcarus
dc.subjectKeywords: Archaean; Asteroid; Atmosphere; Impact; Isotopes; Oxygen; Sulphur
dc.titleArchaean asteroid impacts, banded iron formations and MIF-S anomalies: A discussion
dc.typeJournal article
local.description.notesImported from ARIES
local.identifier.citationvolume207
dc.date.issued2010
local.identifier.absfor020108 - Planetary Science (excl. Extraterrestrial Geology)
local.identifier.ariespublicationf2965xPUB84
local.type.statusPublished Version
local.contributor.affiliationGlikson, Andrew, College of Physical and Mathematical Sciences, ANU
local.description.embargo2037-12-31
local.bibliographicCitation.issue1
local.bibliographicCitation.startpage39
local.bibliographicCitation.lastpage44
local.identifier.doi10.1016/j.icarus.2009.11.024
dc.date.updated2016-02-24T08:33:19Z
local.identifier.scopusID2-s2.0-77950033148
CollectionsANU Research Publications

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