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Reply to the comments by Madsen & Liu on “Late quaternary OSL chronologies from the Qinghai Lake (NE Tibetan Plateau): Inter-comparison of quartz and K-feldspar ages to assess the pre-depositional bleaching”. / Long, Hao; Tsukamoto, Sumiko; Buylaert, Jan-Pieter; Murray, Andrew Sean; Jain, Mayank; Frechen, Manfred.

In: Quaternary Geochronology, Vol. 50, 2019, p. 14-15.

Research output: Contribution to journalComment/debate – Annual report year: 2019Researchpeer-review

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@article{da1b724eb448459d8290c33622eb7727,
title = "Reply to the comments by Madsen & Liu on “Late quaternary OSL chronologies from the Qinghai Lake (NE Tibetan Plateau): Inter-comparison of quartz and K-feldspar ages to assess the pre-depositional bleaching”",
abstract = "In response to the comment of Madsen and Liu (2018), we explain why our quartz optically stimulated luminescence (OSL) ages showing the early MIS 3 lake highstand are robust. We also demonstrate that the difference in the age estimates between ours (Long et al., 2018) and other studies should be attributed to contrasting equivalent dose (De) values, rather than water contents (hence the dose rate) which was claimed by Madsen and Liu (2018).",
author = "Hao Long and Sumiko Tsukamoto and Jan-Pieter Buylaert and Murray, {Andrew Sean} and Mayank Jain and Manfred Frechen",
year = "2019",
doi = "10.1016/j.quageo.2018.11.003",
language = "English",
volume = "50",
pages = "14--15",
journal = "Quaternary Geochronology",
issn = "1871-1014",
publisher = "Elsevier B.V.",

}

RIS

TY - JOUR

T1 - Reply to the comments by Madsen & Liu on “Late quaternary OSL chronologies from the Qinghai Lake (NE Tibetan Plateau): Inter-comparison of quartz and K-feldspar ages to assess the pre-depositional bleaching”

AU - Long, Hao

AU - Tsukamoto, Sumiko

AU - Buylaert, Jan-Pieter

AU - Murray, Andrew Sean

AU - Jain, Mayank

AU - Frechen, Manfred

PY - 2019

Y1 - 2019

N2 - In response to the comment of Madsen and Liu (2018), we explain why our quartz optically stimulated luminescence (OSL) ages showing the early MIS 3 lake highstand are robust. We also demonstrate that the difference in the age estimates between ours (Long et al., 2018) and other studies should be attributed to contrasting equivalent dose (De) values, rather than water contents (hence the dose rate) which was claimed by Madsen and Liu (2018).

AB - In response to the comment of Madsen and Liu (2018), we explain why our quartz optically stimulated luminescence (OSL) ages showing the early MIS 3 lake highstand are robust. We also demonstrate that the difference in the age estimates between ours (Long et al., 2018) and other studies should be attributed to contrasting equivalent dose (De) values, rather than water contents (hence the dose rate) which was claimed by Madsen and Liu (2018).

U2 - 10.1016/j.quageo.2018.11.003

DO - 10.1016/j.quageo.2018.11.003

M3 - Comment/debate

VL - 50

SP - 14

EP - 15

JO - Quaternary Geochronology

JF - Quaternary Geochronology

SN - 1871-1014

ER -