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Article: Quartz thermoluminescence-another potential paleothermometer for sedimentary basin thermal history study

TitleQuartz thermoluminescence-another potential paleothermometer for sedimentary basin thermal history study
Authors
KeywordsApparent age
Basin
Quartz
Thermal regime structure
Thermoluminescence
Issue Date2010
Publisher地球物理学报编辑委员会. The Journal's web site is located at http://www.geophy.cn/CN/volumn/home.shtml
Citation
Chinese Journal Of Geophysics (Acta Geophysica Sinica), 2010, v. 53 n. 1, p. 138-146 How to Cite?
AbstractGood reproducibility of quartz thermal stimulated luminescence phenomenon offers the possibility of dating geological events in subsurface and exploring environmental temperature history as well. As sandstones in basins generally experience one certain pattern of thermal history due to effects of temporal and spatial dependent temperature field, the quartz minerals extracted from these sandstones were evaluated to explore the thermal regime structure information by thermoluminescence analyzing technique. The mean quantitative temperature field information in terms of equivalence for certain burial depths in petroleum basin was investigated using both quartz thermoluminescence apparent age method and laboratory isothermal thermoluminescence simulation measurements. It is recognized that: (1) the variations of both thermoluminescence glow-curve pattern and intensity of certain natural thermoluminescence peaks correlate well with environmental temperature field in corresponding burial depths where the quartz was extracted from. The quartz natural thermoluminescence glow-curves peaks shifting to high temperature and the thermoluminescence intensity reduction result from the increase of both environmental temperature and burial time for quartz due to deepening burial depth; (2) both the additive dose thermoluminescence (TL) and isothermal TL (SA-ITL) techniques were used for quartz mineral TL dating and the resultant apparent ages agree well with each other, and thus one parameter called equivalent temperature was tentatively presented and deducted from apparent TL ages of quartz minerals to evaluate the basin s thermal regime structure information. Quartz thermoluminescence signal can be recognized as one potential paleothermometer if the well correlation of calculated equivalent temperature of buried quartz mineral with other paleothermometers can be supported by more future independent geological evidences.
Persistent Identifierhttp://hdl.handle.net/10722/129177
ISSN
2015 Impact Factor: 0.984
2015 SCImago Journal Rankings: 0.619
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorGong, GLen_HK
dc.contributor.authorLi, SHen_HK
dc.contributor.authorSun, WDen_HK
dc.contributor.authorGuo, Fen_HK
dc.contributor.authorXia, Ben_HK
dc.contributor.authorLü, BFen_HK
dc.date.accessioned2010-12-23T08:33:16Z-
dc.date.available2010-12-23T08:33:16Z-
dc.date.issued2010en_HK
dc.identifier.citationChinese Journal Of Geophysics (Acta Geophysica Sinica), 2010, v. 53 n. 1, p. 138-146en_HK
dc.identifier.issn0001-5733en_HK
dc.identifier.urihttp://hdl.handle.net/10722/129177-
dc.description.abstractGood reproducibility of quartz thermal stimulated luminescence phenomenon offers the possibility of dating geological events in subsurface and exploring environmental temperature history as well. As sandstones in basins generally experience one certain pattern of thermal history due to effects of temporal and spatial dependent temperature field, the quartz minerals extracted from these sandstones were evaluated to explore the thermal regime structure information by thermoluminescence analyzing technique. The mean quantitative temperature field information in terms of equivalence for certain burial depths in petroleum basin was investigated using both quartz thermoluminescence apparent age method and laboratory isothermal thermoluminescence simulation measurements. It is recognized that: (1) the variations of both thermoluminescence glow-curve pattern and intensity of certain natural thermoluminescence peaks correlate well with environmental temperature field in corresponding burial depths where the quartz was extracted from. The quartz natural thermoluminescence glow-curves peaks shifting to high temperature and the thermoluminescence intensity reduction result from the increase of both environmental temperature and burial time for quartz due to deepening burial depth; (2) both the additive dose thermoluminescence (TL) and isothermal TL (SA-ITL) techniques were used for quartz mineral TL dating and the resultant apparent ages agree well with each other, and thus one parameter called equivalent temperature was tentatively presented and deducted from apparent TL ages of quartz minerals to evaluate the basin s thermal regime structure information. Quartz thermoluminescence signal can be recognized as one potential paleothermometer if the well correlation of calculated equivalent temperature of buried quartz mineral with other paleothermometers can be supported by more future independent geological evidences.en_HK
dc.languagechien_US
dc.publisher地球物理学报编辑委员会. The Journal's web site is located at http://www.geophy.cn/CN/volumn/home.shtmlzh_HK
dc.relation.ispartofChinese Journal of Geophysics (Acta Geophysica Sinica)en_HK
dc.subjectApparent ageen_HK
dc.subjectBasinen_HK
dc.subjectQuartzen_HK
dc.subjectThermal regime structureen_HK
dc.subjectThermoluminescenceen_HK
dc.titleQuartz thermoluminescence-another potential paleothermometer for sedimentary basin thermal history studyen_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=0001-5733&volume=53&issue=1&spage=138&epage=146&date=2010&atitle=Quartz+thermoluminescence+-+another+potential+paleothermometer+for+sedimentary+basin+thermal+history+study-
dc.identifier.emailLi, SH:shli@hku.hken_HK
dc.identifier.authorityLi, SH=rp00740en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.3969/j.issn.0001-5733.2010.01.015en_HK
dc.identifier.scopuseid_2-s2.0-77953865847en_HK
dc.identifier.hkuros177682en_US
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-77953865847&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume53en_HK
dc.identifier.issue1en_HK
dc.identifier.spage138en_HK
dc.identifier.epage146en_HK
dc.identifier.isiWOS:000274274500015-
dc.publisher.placeChinaen_HK
dc.identifier.scopusauthoridGong, GL=7103214935en_HK
dc.identifier.scopusauthoridLi, SH=24438103700en_HK
dc.identifier.scopusauthoridSun, WD=7404011201en_HK
dc.identifier.scopusauthoridGuo, F=35227305400en_HK
dc.identifier.scopusauthoridXia, B=36112247900en_HK
dc.identifier.scopusauthoridLü, BF=36175067700en_HK

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