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dc.contributor.authorAugustsson, Carita
dc.date.accessioned2023-02-16T11:31:01Z
dc.date.available2023-02-16T11:31:01Z
dc.date.created2021-05-10T10:11:12Z
dc.date.issued2021
dc.identifier.citationAugustsson, C. (2021). Influencing factors on petrography interpretations in provenance research—A case-study review. Geosciences, 11(5), 205.en_US
dc.identifier.issn2076-3263
dc.identifier.urihttps://hdl.handle.net/11250/3051455
dc.description.abstractThe use of framework petrography is a common initial step in provenance research of sand and sandstone. The data tend to be interpreted based on the three main components quartz, feldspar, and lithic fragments. Surprisingly often, this is done without taking other influencing factors than the tectonic setting of the catchment and/or the surroundings of the depositional basin into account. Based on a database of 14 studies with approximately 900 petrographic data points from sand and sandstone, this study demonstrates quantitative effects on the apparent composition resulting from both geological and non-geological biases. The study illustrates sandstone-classification differences based on different specifications of the three end-members quartz, feldspar, and lithic or rock fragments, how the point-counting method can affect the apparent petrographic composition of sandstone, how sorting and facies bias may be differentiated from a climate or provenance signal, and how bias due to diagenetic effects can be minimised. In conclusion, both geological and non-geological biases should be considered for provenance studies that include petrographic data.en_US
dc.language.isoengen_US
dc.publisherMDPIen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleInfluencing factors on petrography interpretations in provenance research – a case-study reviewen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holderThe authoren_US
dc.subject.nsiVDP::Matematikk og Naturvitenskap: 400en_US
dc.source.pagenumber25en_US
dc.source.volume11en_US
dc.source.journalGeosciencesen_US
dc.identifier.doi10.3390/geosciences11050205
dc.identifier.cristin1909084
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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