High resolution dating of loess profile from Biały KoŚciół, south-west Poland

Piotr Moska; Grzegorz Adamiec; Zdzisław Jary

doi:10.1016/j.quageo.2012.04.003

High resolution dating of loess profile from Biały KoŚciół, south-west Poland

Piotr Moska
, Grzegorz Adamiec
, Zdzisław Jary

Zakład Geochronologii i Badań Izotopowych Środowiska (RIF/RIF2)

University of Wrocław

Wyniki badań: Wkład do czasopisma › Artykuł › recenzja

26 Cytowania z bazy Scopus

Abstrakt

Results of high resolution optically stimulated luminescence (OSL) dating of one of the most complex loess/palaeosol complex in Poland located in the vicinity of the village Biały KoŚciół (south-west Poland) are presented. Twenty one samples were collected from the 9-m loess profile and dated using the single-aliquot regenerative method applied to coarse grained quartz fraction (90-125 μm). The obtained single-aliquot results were analysed using the central age model. OSL ages are in good agreement with the chronology inferred from the marine oxygen isotope (MOIS) stratigraphy and ages reported for similar lithostratigraphic units for other loess profiles in Europe. However, for the deepest part of the profile underestimation of OSL is observed.

Język oryginału	angielski
Strony (od–do)	87-93
Liczba stron	7
Czasopismo	Quaternary Geochronology
Tom	10
Identyfikatory DOI	https://doi.org/10.1016/j.quageo.2012.04.003
Status publikacji	Opublikowano - lip 2012

Obszary tematyczne ASJC Scopus

Geologia
Stratygrafia
Nauki o Ziemi i planetach (różne)

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10.1016/j.quageo.2012.04.003

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title = "High resolution dating of loess profile from Bia{\l}y Ko{\'S}ci{\'o}{\l}, south-west Poland",

abstract = "Results of high resolution optically stimulated luminescence (OSL) dating of one of the most complex loess/palaeosol complex in Poland located in the vicinity of the village Bia{\l}y Ko{\'S}ci{\'o}{\l} (south-west Poland) are presented. Twenty one samples were collected from the 9-m loess profile and dated using the single-aliquot regenerative method applied to coarse grained quartz fraction (90-125 μm). The obtained single-aliquot results were analysed using the central age model. OSL ages are in good agreement with the chronology inferred from the marine oxygen isotope (MOIS) stratigraphy and ages reported for similar lithostratigraphic units for other loess profiles in Europe. However, for the deepest part of the profile underestimation of OSL is observed.",

keywords = "Equivalent dose, Luminescence dating, Polish loess stratigraphy, Quartz",

author = "Piotr Moska and Grzegorz Adamiec and Zdzis{\l}aw Jary",

year = "2012",

month = jul,

doi = "10.1016/j.quageo.2012.04.003",

language = "English",

volume = "10",

pages = "87--93",

journal = "Quaternary Geochronology",

issn = "1871-1014",

publisher = "Elsevier B.V.",

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TY - JOUR

T1 - High resolution dating of loess profile from Biały KoŚciół, south-west Poland

AU - Moska, Piotr

AU - Adamiec, Grzegorz

AU - Jary, Zdzisław

PY - 2012/7

Y1 - 2012/7

N2 - Results of high resolution optically stimulated luminescence (OSL) dating of one of the most complex loess/palaeosol complex in Poland located in the vicinity of the village Biały KoŚciół (south-west Poland) are presented. Twenty one samples were collected from the 9-m loess profile and dated using the single-aliquot regenerative method applied to coarse grained quartz fraction (90-125 μm). The obtained single-aliquot results were analysed using the central age model. OSL ages are in good agreement with the chronology inferred from the marine oxygen isotope (MOIS) stratigraphy and ages reported for similar lithostratigraphic units for other loess profiles in Europe. However, for the deepest part of the profile underestimation of OSL is observed.

AB - Results of high resolution optically stimulated luminescence (OSL) dating of one of the most complex loess/palaeosol complex in Poland located in the vicinity of the village Biały KoŚciół (south-west Poland) are presented. Twenty one samples were collected from the 9-m loess profile and dated using the single-aliquot regenerative method applied to coarse grained quartz fraction (90-125 μm). The obtained single-aliquot results were analysed using the central age model. OSL ages are in good agreement with the chronology inferred from the marine oxygen isotope (MOIS) stratigraphy and ages reported for similar lithostratigraphic units for other loess profiles in Europe. However, for the deepest part of the profile underestimation of OSL is observed.

KW - Equivalent dose

KW - Luminescence dating

KW - Polish loess stratigraphy

KW - Quartz

UR - https://www.scopus.com/pages/publications/84863774908

U2 - 10.1016/j.quageo.2012.04.003

DO - 10.1016/j.quageo.2012.04.003

M3 - Article

AN - SCOPUS:84863774908

SN - 1871-1014

VL - 10

SP - 87

EP - 93

JO - Quaternary Geochronology

JF - Quaternary Geochronology

ER -

High resolution dating of loess profile from Biały KoŚciół, south-west Poland

Abstrakt

Obszary tematyczne ASJC Scopus

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