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Relevant bibliographies by topics / Geology, Stratigraphic Optically stimulated luminescence dating

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Academic literature on the topic 'Geology, Stratigraphic Optically stimulated luminescence dating'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Geology, Stratigraphic Optically stimulated luminescence dating"

1

Jeong, Gi Young, Chang-Sik Cheong, and Jeong-Heon Choi. "The effect of weathering on optically stimulated luminescence dating." Quaternary Geochronology 2, no. 1-4 (January 2007): 117–22. http://dx.doi.org/10.1016/j.quageo.2006.05.023.

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Lüthgens, Christopher, Matthias Krbetschek, Margot Böse, and Margret C. Fuchs. "Optically stimulated luminescence dating of fluvioglacial (sandur) sediments from north-eastern Germany." Quaternary Geochronology 5, no. 2-3 (April 2010): 237–43. http://dx.doi.org/10.1016/j.quageo.2009.06.007.

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Mischke, Steffen, Zhongping Lai, Bernhard Aichner, Liv Heinecke, Zafar Mahmoudov, Marie Kuessner, and Ulrike Herzschuh. "Radiocarbon and optically stimulated luminescence dating of sediments from Lake Karakul, Tajikistan." Quaternary Geochronology 41 (August 2017): 51–61. http://dx.doi.org/10.1016/j.quageo.2017.05.008.

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4

Armitage, S. J., and R. C. Pinder. "Testing the applicability of optically stimulated luminescence dating to Ocean Drilling Program cores." Quaternary Geochronology 39 (April 2017): 124–30. http://dx.doi.org/10.1016/j.quageo.2017.02.008.

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5

NIELSEN, A., A. MURRAY, M. PEJRUP, and B. ELBERLING. "Optically stimulated luminescence dating of a Holocene beach ridge plain in Northern Jutland, Denmark." Quaternary Geochronology 1, no. 4 (December 2006): 305–12. http://dx.doi.org/10.1016/j.quageo.2006.03.001.

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Bailiff, I. K., D. Bridgland, and Pedro P. Cunha. "Extending the range of optically stimulated luminescence dating using vein-quartz and quartzite sedimentary pebbles." Quaternary Geochronology 65 (August 2021): 101180. http://dx.doi.org/10.1016/j.quageo.2021.101180.

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STEVENS, THOMAS, and HUAYU LU. "Optically stimulated luminescence dating as a tool for calculating sedimentation rates in Chinese loess: comparisons with grain-size records." Sedimentology 56, no. 4 (June 2009): 911–34. http://dx.doi.org/10.1111/j.1365-3091.2008.01004.x.

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Pears, Ben, Antony G. Brown, Phillip S. Toms, Jamie Wood, David Sanderson, and Richard Jones. "A sub-centennial-scale optically stimulated luminescence chronostratigraphy and late Holocene flood history from a temperate river confluence." Geology 48, no. 8 (May 18, 2020): 819–25. http://dx.doi.org/10.1130/g47079.1.

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Abstract River confluences can be metastable and contain valuable geological records of catchment response to decadal- to millennial-scale environmental change. However, in alluvial reaches, flood stratigraphies are particularly hard to date using 14C. In this paper, we use a novel combination of optically stimulated luminescence and multiproxy sedimentological analyses to provide a flood record for the confluence of the Rivers Severn and Teme (United Kingdom) over the past two millennia, which we compare with independent European climate records. The results show that by ca. 2000 yr B.P., the Severn-Teme confluence had stabilized and overbank alluviation had commenced. Initially, this occurred from moderately high flood magnitudes between ca. 2000 and 1800 yr B.P. (50 BCE–150 CE), but was followed from 1800 to 1600 yr B.P. (150–350 CE) by fine alluvial deposition and decreased flood intensity. From 1600 to 1400 yr B.P. (350–550 CE), the accumulation rate increased, with evidence of large flood events associated with the climatic deterioration of the Dark Age Cold Period. Following a period of reduced flood activity after ca. 1400 yr B.P. (ca. 550 CE), larger flood events and increase in accumulation rate once again became more prevalent from ca. 850 yr B.P. (ca. 1100 CE), coincident with the start of the Medieval Climate Anomaly, a period associated with warmer, wetter conditions and increased land-use intensity. This state persisted until ca. 450 yr B.P. (ca. 1500 CE), after which increased flood magnitudes can be associated with climatic variations during the Little Ice Age. We demonstrate that from the combination of high-resolution dating techniques and multiple analytical parameters, distinctive phases of relative flood magnitude versus flood duration can be determined to a detailed chronological precision beyond that possible from 14C dating. This permits the identification of the regional factors behind floodplain sedimentation, which we correlate with the intensification of land-use and climatic drivers over the last two millennia.

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Frechen, M., K. Vanneste, K. Verbeeck, E. Paulissen, and T. Camelbeeck. "The Deposition History of the Coversands along the Bree Fault Escarpment, NE Belgium." Netherlands Journal of Geosciences 80, no. 3-4 (December 2001): 171–85. http://dx.doi.org/10.1017/s0016774600023829.

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AbstractThe coversands along the Bree fault escarpment, NE Belgium, were investigated by a combined dating approach including infrared optically stimulated luminescence (IRSL), thermoluminescence (TL) and radiocarbon methods. Four trenches were excavated cutting the fault scarp near the village of Bree in northeast Belgium. Altogether 17 luminescence samples and seven radiocarbon samples were investigated in order to set up a more reliable and precise chronological frame for the local coversand stratigraphy and the timing of Late Quaternary earthquake events. The chronological results indicate at least five accumulation periods for the coversand units in the area of interest. The oldest coversands were deposited during Saalian or Early Weichselian followed by coversands deposited during the Early and/or Middle Weichselian. At least three coversand units can be distinguished for the time span of the Late Weichselian to Holocene. Significant TL age underestimation of more than 20% compared to IRSL was found for samples from Trench 4. Most of the IRSL age estimates are in agreement with radiocarbon dates from the same section.

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Pietsch, Timothy John. "Optically stimulated luminescence dating of young (<500 years old) sediments: Testing estimates of burial dose." Quaternary Geochronology 4, no. 5 (October 2009): 406–22. http://dx.doi.org/10.1016/j.quageo.2009.05.013.

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Dissertations / Theses on the topic "Geology, Stratigraphic Optically stimulated luminescence dating"

1

Ballarini, Mirko. "Optical dating of quartz from young deposits : from single-aliquot to single-grain : proefschrift ... door /." Amsterdam : Fairfax, VA : Delft University Press ; IOS Press [distributor], 2006. http://www.loc.gov/catdir/toc/fy0714/2006279690.html.

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Li, Bo. "Development and application of optical dating using quartz and potassium-feldspar from quaternary sediments." Click to view the E-thesis via HKUTO, 2007. http://sunzi.lib.hku.hk/HKUTO/record/B39557212.

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Fan, Anchuan, and 范安川. "Quartz OSL dating of quaternary sediments from China." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2010. http://hub.hku.hk/bib/B45700187.

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Lee, Ting Jennifer. "Holocene evolution of a hypersaline lake Lagkor Tso, western Tibet /." Click to view the E-thesis via HKUTO, 2008. http://sunzi.lib.hku.hk/hkuto/record/B39634140.

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Li, Bo, and 李波. "Development and application of optical dating using quartz and potassium-feldspar from quaternary sediments." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2007. http://hub.hku.hk/bib/B39557212.

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Gong, Zhijun, and 龚志军. "Application of optical dating to late quaternary uplift and thrust activity in the northern piedmont of Tian Shan, China." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2012. http://hdl.handle.net/10722/193394.

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Tian Shan is one of the most important orogenic belts in central Asia. It has been reactivated as a result of the Cenozoic India-Eurasia collision. Dating of the late Cenozoic tectonic deformation of Tian Shan and its piedmonts is important for understanding the mountain building as well as evaluating seismic hazards in the region. This study is focused on the applications of optical dating to the late Quaternary uplift and thrust activity along Manas River, in the northern piedmont of the Tian Shan, China. The sediments on river terraces were dated with optical dating. The elevations were measured with the kinematic global position system (GPS). The results suggest that two phases can be identified according to the significantly different river incision rates. One phase was from ~20 ka to ~4.8 ka, with a much slower incision rate of ~ 2.2 ± 0.6 mm/yr. The other phase was from ~4.8 ka to present, with a faster incision rate of ~ 13.5 ± 0.6 mm/yr. The accelerated incision rate of Manas River was mainly attributed to the tectonic forces, suggesting that the tectonic uplift was significantly intensified since ~4.8 ka in the northern piedmont of Tian Shan. The study region has suffered from multiple thrust activities during the late Quaternary, which led to the intensive deformations of the river terraces. By studying the deformed terraces, I evaluated the timing of the past thrust activities as well as the vertical slip rate of the thrust faults. The results demonstrated that the thrust activity intensified during the late Holocene, as manifested by the more frequent thrust activities and higher vertical slip rates. Both quartz and potassium feldspar can be as dosimeters for optical dating of sediments. However, quartz OSL is sometimes seriously impeded with problems such as very dim signals and insufficient bleaching problems. K-feldspar has attractive advantages over quartz, despite of problem of anomalous fading. K-feldspar was explored in this study, by investigating the relationship between the infrared stimulated luminescence (IRSL) and blue light stimulated luminescence (BLSL) signals. For IRSL and BLSL at 60 °C, it was suggested that most of the IRSL could be bleached by blue light (BL), while the BLSL could only be partially bleached by infrared (IR) stimulation. Besides, the fast and medium components of BLSL were mainly associated with the IRSL. If IR stimulation temperature was raised from 60 to 200 °C, at least two portions of the IRSL signals at 200 °C were observed. One portion could be bleached by BL at 60 °C and the other portion was hardly bleached by BL at 60 °C. Dating of K-feldspar from the various signals provided cross-checking for the reliability of quartz OSL for dating sedimentary samples.
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7

Summa, Michelle Carlene. "Geologic Mapping, Alluvial Stratigraphy, and Optically Stimulated Luminescence Dating of the Kanab Creek Area, Southern Utah." DigitalCommons@USU, 2009. https://digitalcommons.usu.edu/etd/506.

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At the turn of the century, Kanab Creek incised 30-meters into its alluvium, leaving behind fluvial terraces and thick basin fill sediments exposed along arroyo walls. Research objectives were to determine the timing and causes of past valley-filling and arroyo-cutting episodes along a 20 km-long reach of Kanab Creek in southern Utah. Fluvial deposits were mapped at the 1:12,000 scale and sediments were described and dated using Optically Stimulated Luminescence (OSL) and radiocarbon dating. The Kanab Creek valley can be divided into a narrow, upper terraced reach and a broad lower basin fill reach near Kanab, Utah. The most prominent terrace in the upper reach is Quaternary alluvial terrace 4 (Qat4), followed by Qat3, Qat2/3, and Qat2 map units. These are composed of tabular-bedded, fine-grained sand, silt, and clay layers. The Qat2/3 map unit is a both a fill and fill-cut terrace underlain by Qa4, Qa3, and Qa2 alluvium and is used when the Qat3 fill-cut (fill-strath) terrace can not be differentiated from the Qat2 fill terrace due to their similar geomorphic position. The Qat3 fill-cut terrace upstream correlates to ~8 meters of aggradation downstream. The youngest terrace, Qat1, is a minor terrace, composed of coarse-grained channel facies. More recent channel and floodplain deposits were deposited over the last century following arroyo cutting. OSL and radiocarbon results suggest at least four cycles of fluvial cutting and filling: >6-3.5ka (Qa4), ~3->1ka (Qa3), 0.7-0.12ka (Qa2), and post-1880 AD (Qa1). Correlation to regional climate records suggests major periods of aggradation correlate to regionally cooler and wetter climatic intervals. Periods of arroyo cutting occurred at >6ka, ~3ka, 1-0.7ka, and during historic arroyo cutting (1882-1914 AD), and correlate to regionally warmer, drier intervals. These periods of aggradation and incision are roughly contemporaneous with regional drainages, except for the large aggradation seen in Kanab Creek 6-3.5ka (Qa4). Analysis of terrace longitudinal profiles indicates Qat4 has the lowest concavity suggesting that Qat4 aggraded during a period of greater sediment supply and/or reduced flood regime. Although OSL samples exhibited some degree of incomplete zeroing, calculated ages using a minimum age model are consistent with radiocarbon results.

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8

Lee, Ting Jennifer, and 李婷. "Holocene evolution of a hypersaline lake: Lagkor Tso, western Tibet." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2008. http://hub.hku.hk/bib/B39634140.

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9

Pietsch, Timothy J. "Fluvial geomorphology and late quaternary geochronology of the Gwydir fan-plain." Access electronically, 2005. http://www.library.uow.edu.au/adt-NWU/public/adt-NWU20060720.153247/index.html.

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10

Short, Michael Anthony. "Some aspects of optically stimulated luminescence for sediment dating." Thesis, [Hong Kong : University of Hong Kong], 1993. http://sunzi.lib.hku.hk/hkuto/record.jsp?B13645985.

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Books on the topic "Geology, Stratigraphic Optically stimulated luminescence dating"

1

Ballarini, Mirko. Optical dating of quartz from young deposits: From single-aliquot to single-grain : proefschrift ... Delft: Delft University Press, 2006.

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Conference papers on the topic "Geology, Stratigraphic Optically stimulated luminescence dating"

1

Garcia, Antonio F., Daniel Dean, and Shannon A. Mahan. "DEDUCING GEOMORPHIC PROCESS AND THE CHARACTER OF PALEOCLIMATE FROM SURFICIAL GEOLOGY AND GEOCHRONOLOGY BASED ON OPTICALLY STIMULATED LUMINESCENCE (OSL) DATING." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-298356.

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