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Authigenic or detrital origin of pyrrhotite in sediments?: Resolving a paleomagnetic conundrum

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dc.contributor.authorHorng, Chorng-Shern
dc.contributor.authorRoberts, Andrew
dc.date.accessioned2015-12-07T22:30:58Z
dc.date.issued2006
dc.date.updated2015-12-07T10:11:28Z
dc.description.abstractMonoclinic pyrrhotite (Fe7S8) is widely claimed to carry magnetizations acquired during early diagenesis in anoxic sedimentary environments. In contrast, geochemical literature indicates that pyrrhotite formation is extremely slow below 180 °C, which mak
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/1885/22568
dc.publisherElsevier
dc.sourceEarth and Planetary Science Letters
dc.subjectKeywords: Authigenic; Diagenesis; Iron sulphide; Monoclinic; Pyrrhotite; Geochemistry; Magnetization; Metamorphic rocks; Remanence; Sediments; Sulfide minerals; paleomagnetism; pyrrhotite; sediment chemistry Authigenic; Detrital; Diagenesis; Hexagonal; Iron sulphide; Monoclinic; Pyrrhotite
dc.titleAuthigenic or detrital origin of pyrrhotite in sediments?: Resolving a paleomagnetic conundrum
dc.typeJournal article
local.bibliographicCitation.lastpage762
local.bibliographicCitation.startpage750
local.contributor.affiliationHorng, Chorng-Shern, Academia Sinica
local.contributor.affiliationRoberts, Andrew, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidRoberts, Andrew, u4817957
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040406 - Magnetism and Palaeomagnetism
local.identifier.ariespublicationu4539375xPUB22
local.identifier.citationvolume241
local.identifier.doi10.1016/j.epsl.2005.11.008
local.identifier.scopusID2-s2.0-30744449289
local.type.statusPublished Version

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