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Low temperature thermochronology using thermoluminescence signals from K-feldspar

potentials of luminescence thermochronology, it has not been widely applied because suitable dating protocols that can be routinely and conveniently applied in the laboratory are unavailable. Guralnik et al . (2015) studied the OSL signals from quartz samples and found undesirable OSL characteristics for dating the rocks. King et al . (2016) studied the infra-red stimulated luminescence (IRSL) signals from K-feldspar through the multi-elevated-temperature (MET) protocol ( Li and Li, 2011 ), and indicated the great potential of it. Tang and Li (2015) suggested that

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Aspects of Infrared Radioluminescence dosimetry in K-feldspar

[1] Buylaert JP, Jain M, Murray AS, Thomsen KJ and Lapp T, 2012. IR-RF dating of sand-sized k-feldspar extracts: A test of accuracy. Radiation Measurements 47(9): 759–765, DOI 10.1016/j.radmeas.2012.06.021. http://dx.doi.org/10.1016/j.radmeas.2012.06.021 [2] Erfurt G and Krbetschek MR, 2003. IRSAR — a single-aliquot regenerative-dose dating protocol applied to the infrared radiofluorescence (IRRF) of coarse-grain k-feldspar. Ancient TL 21(1): 35. [3] Krbetschek MR, Trautmann T, Dietrich

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Comparison of three K-feldspar luminescence dating methods for Holocene samples

by a Monte-Carlo method. Quaternary Science Reviews 18: 231–234, DOI 10.1016/S0277-3791(98)00056-0. http://dx.doi.org/10.1016/S0277-3791(98)00056-0 [11] Huntley DJ and Lamothe M, 2001. Ubiquity of anomalous fading in K-feldspars and the measurement and correction for it in optical dating. Canadian Journal of Earth Sciences 38: 1093–1106, DOI 10.1139/cjes-38-7-1093. http://dx.doi.org/10.1139/cjes-38-7-1093 [12] Huntley DJ and Lian OB, 2006. Some observations on tunnelling of trapped electrons in feldspars and their

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Stability of IRSL signals from sedimentary K-feldspar samples

[1] Buylaert JP, Murray AS and Huot S, 2008. Optical dating of an Eemian site in Northern Russia using K-feldspar. Radiation Measurements 43: 715–720, DOI 10.1016/j.radmeas.2008.01.027. http://dx.doi.org/10.1016/j.radmeas.2008.01.027 [2] Buylaert JP, Murray AS and Thomsen KJ, 2009. Testing the potential of an elevated temperature IRSL signal from K-feldspar. Radiation Measurements 44: 560–565, DOI 10.1016/j.radmeas.2009.02.007. http://dx.doi.org/10.1016/j.radmeas.2009.02.007 [3] Buylaert

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Quartz OSL and K-feldspar post-IR IRSL dating of sand accumulation in the Lower Liao Plain (Liaoning, NE China)

sand deposition are discussed. Our second aim is to investigate the effects of the residual dose in the pIRIR dating of young sediments. The pIRIR 150 protocol is applied on K-feldspar fraction for all samples and the results are compared with the quartz ages to determine the applicability of the protocol for the young dune sediments. 2 Study area, site description, and sampling Study area The Lower Liao Plain (LLP) is an alluvial plain located in northeastern China (Fig. 1) . To the north of the LLP, the Horqin dune field is located, which is one of the

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Residual doses and sensitivity change of post IR IRSL signals from potassium feldspar under different bleaching conditions

[1] Aitken MJ, 1998. An Introduction to Optical Dating. Oxford, Oxford University Press: 359pp. [2] Bøtter-Jensen L, Bulur E, Duller GAT and Murray AS, 2000. Advances in luminescence instrument systems. Radiation Measurements 32(5–6): 523–528, DOI 10.1016/S1350-4487(00)00039-1. http://dx.doi.org/10.1016/S1350-4487(00)00039-1 [3] Buylaert JP, Murray AS, Thomsen KJ and Jain M, 2009. Testing the potential of an elevated temperature IRSL signal from K-feldspar. Radiation Measurements 44

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Luminescence dating of young coastal deposits from New Zealand using feldspar

M, 2009. Testing the potential of an elevated temperature IRSL signal from K-feldspar. Radiation Measurements 44(5–6): 560–565, DOI 10.1016/j.radmeas.2009.02.007. http://dx.doi.org/10.1016/j.radmeas.2009.02.007 [10] Buylaert JP, Huot S, Murray AS and Van den Haute P, 2011. Infrared stimulated luminescence dating of an Eemian (MIS 5e) site in Denmark using K-feldspar. Boreas 40(1): 46–56, DOI 10.1111/j.1502-3885.2010.00156.x. http://dx.doi.org/10.1111/j.1502-3885.2010.00156.x [11] Cooper AF and Kostro F, 2006. A

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Chronology of Cauvery Delta Sediments from Shallow Subsurface Cores Using Elevated-Temperature Post-IR IRSL Dating of Feldspar

. Quaternary International 189(1): 5-38, DOI 10.1016/j.quaint.2007.08.036. Buylaert JP, Murray AS, Thomsen KJ and Jain M, 2009. Testing the potential of an elevated temperature IRSL signal from K-feldspar. Radiation Measurements 44: 560-565, DOI 10.1016/j.radmeas.2009.02.007. Chandra K, Philip PC, Sridharan P, Chopra VS, Brahmaji Rao and Saha PK, 1991. Petroleum source-rock potentials of the cretaceous transgressive-regressive sedimentary sequences of the Cauvery Basin. Journal of Southeast Asian Earth Sciences 5

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Overcoming Environmental Dose Rate Changes in Luminescence Dating of Waterlain Deposits

Dosimetry 101(1-4): 333-338. Zhao H and Li S-H, 2005. Internal dose rate to K-feldspar grains from radioactive elements other than potassium. Radiation Measurements 40(1): 84-93, DOI 10.1016/j.radmeas.2004.11.004 Huntley DJ and Lamothe M, 2001. Ubiquity of anomalous fading in K-feldspars and the measurement and correction for it in optical dating. Canadian Journal of Earth Sciences 38(7): 1093-1106, DOI 10.1139/cjes-38-7-1093. Huot S and Lamothe M, 2003. Variability of infrared stimulated

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Luminescence dating of Holocene beach-ridge sands on the Yumigahama Peninsula, western Japan

activity on the geomorphology of this region. Although optically stimulated luminescence (OSL) of quartz grains has generally been the first choice for dating Holocene coastal deposits, problems related to the OSL properties of quartz have been reported from many regions of Japan (e.g., Tsukamoto et al , 2003 ; Watanuki et al , 2005 ; Tokuyasu et al ., 2010 ; Tamura et al ., 2011 , 2015 ). The use of post-infrared (post-IR) infrared stimulated luminescence (IRSL) of K-feldspar at relatively low temperatures ( Thomsen et al , 2008 ; Reimann et al , 2011b

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