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Article: Age dependence of luminescence signals from granitic and mylonitic quartz

TitleAge dependence of luminescence signals from granitic and mylonitic quartz
Authors
Issue Date1997
PublisherPergamon. The Journal's web site is located at http://www.elsevier.com/locate/quascirev
Citation
Quaternary Science Reviews, 1997, v. 16 n. 3-5, p. 427-430 How to Cite?
AbstractGranite and mylonitic samples with an age range of 11-3300 Ma were collected from different regions of China. Several luminescence signals were measured from the extracted quartz. Age-dependence has been observed in their luminescence signals, including the sensitivity of the 110°C TL-peak, the temperature of the high-temperature TL peak and the regenerated TL with β dose. Other luminescence signals show little age-dependence. The TL reaches maximum at about 160°C in the quartz samples, which is significantly different from signals from sediments. It is concluded that the luminescence signals may lead to the establishment of a new geochronological method for the whole earth history.
Persistent Identifierhttp://hdl.handle.net/10722/90473
ISSN
2015 Impact Factor: 4.521
2015 SCImago Journal Rankings: 2.928
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorHan, Z-
dc.contributor.authorLi, SH-
dc.contributor.authorTso, MYW-
dc.date.accessioned2010-09-06T10:11:05Z-
dc.date.available2010-09-06T10:11:05Z-
dc.date.issued1997-
dc.identifier.citationQuaternary Science Reviews, 1997, v. 16 n. 3-5, p. 427-430-
dc.identifier.issn0277-3791-
dc.identifier.urihttp://hdl.handle.net/10722/90473-
dc.description.abstractGranite and mylonitic samples with an age range of 11-3300 Ma were collected from different regions of China. Several luminescence signals were measured from the extracted quartz. Age-dependence has been observed in their luminescence signals, including the sensitivity of the 110°C TL-peak, the temperature of the high-temperature TL peak and the regenerated TL with β dose. Other luminescence signals show little age-dependence. The TL reaches maximum at about 160°C in the quartz samples, which is significantly different from signals from sediments. It is concluded that the luminescence signals may lead to the establishment of a new geochronological method for the whole earth history.-
dc.languageeng-
dc.publisherPergamon. The Journal's web site is located at http://www.elsevier.com/locate/quascirev-
dc.relation.ispartofQuaternary Science Reviews-
dc.rightsNOTICE: this is the author’s version of a work that was accepted for publication in [Journal title]. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in PUBLICATION, [VOL#, ISSUE#, (DATE)] DOI#-
dc.titleAge dependence of luminescence signals from granitic and mylonitic quartz-
dc.typeArticle-
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=1871-1014&volume=16&issue=3-5&spage=427&epage=430&date=1997&atitle=Age+dependence+of+luminescence+signals+from+granitic+and+mylonitic+quartzen_HK
dc.identifier.emailLi, SH: shli@hku.hk-
dc.identifier.emailTso, MYW: mmytso@hkuccc.hku.hk-
dc.identifier.authorityLi, SH=rp00740-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1016/S0277-3791(96)00107-2-
dc.identifier.scopuseid_2-s2.0-0030909087en_HK
dc.identifier.hkuros25797-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-0030909087&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume16-
dc.identifier.issue3-5-
dc.identifier.spage427-
dc.identifier.epage430-
dc.identifier.isiWOS:A1997XG29900020-
dc.publisher.placeUnited Kingdom-
dc.identifier.scopusauthoridHan, ZY=7402859525en_HK
dc.identifier.scopusauthoridLi, SH=24438103700en_HK
dc.identifier.scopusauthoridTso, MYW=7102052118en_HK

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