Applicability of a quartz OSL standardised growth curve for D-edetermination up to 400 Gy for lacustrine sediments from the QaidamBasin of the Qinghai-Tibetan Plateau

ISL OpenIR > 青海盐湖研究所知识仓储

	Applicability of a quartz OSL standardised growth curve for D-edetermination up to 400 Gy for lacustrine sediments from the QaidamBasin of the Qinghai-Tibetan Plateau
	Long, Hao; Lai, ZhongPing; Fan, QiShun; Sun, YongJuan; Liu, XiangJun
	2010
发表期刊	QUATERNARY GEOCHRONOLOGY
ISSN	1871-1014
卷号	5 期号:2-3 页码:212-217
摘要	The standardised growth curve (SGC) for quartz OSL has recently been developed as a practical means to reduce measurement times when determining palaeodoses using quartz of aeolian sediments, especially loess and desert sand from the same section or the same geographical area. In the present study, we test the performance of SGCs for lacustrine sediments of three cores in the Qaidam Basin of the Qinghai-Tibetan Plateau (QTP) in China. A total of nine samples were collected (three samples from each of the three cores), and silt-sized (38-63 mu m) quartz was extracted for the experiment. The results demonstrated that: (a) Nine samples display similar dose-response curves up to a regeneration dose of 600 Gy using single aliquot regenerative-dose (SAR) protocol, suggesting the existence of a standardised growth curve for lacustrine sediments in the Qaidam Basin; (b) For samples with D(e)s of up to 400 Gy, the Des determined by the SGC are in agreement with the D(e)s by the SAR protocol, suggesting that the SGC approach could be used for D-e determination up to a dose of 400 Gy for lacustrine samples from the Qaidam Basin of the Qinghai-Tibetan Plateau in China; (c) The saturation dose for these samples is more than 600 Gy, and in the growth curve a linear growth part was observed in the high dose range of >200 Gy. (C) 2009 Elsevier B.V. All rights reserved. The standardised growth curve (SGC) for quartz OSL has recently been developed as a practical means to reduce measurement times when determining palaeodoses using quartz of aeolian sediments, especially loess and desert sand from the same section or the same geographical area. In the present study, we test the performance of SGCs for lacustrine sediments of three cores in the Qaidam Basin of the Qinghai-Tibetan Plateau (QTP) in China. A total of nine samples were collected (three samples from each of the three cores), and silt-sized (38-63 mu m) quartz was extracted for the experiment. The results demonstrated that: (a) Nine samples display similar dose-response curves up to a regeneration dose of 600 Gy using single aliquot regenerative-dose (SAR) protocol, suggesting the existence of a standardised growth curve for lacustrine sediments in the Qaidam Basin; (b) For samples with D(e)s of up to 400 Gy, the Des determined by the SGC are in agreement with the D(e)s by the SAR protocol, suggesting that the SGC approach could be used for D-e determination up to a dose of 400 Gy for lacustrine samples from the Qaidam Basin of the Qinghai-Tibetan Plateau in China; (c) The saturation dose for these samples is more than 600 Gy, and in the growth curve a linear growth part was observed in the high dose range of >200 Gy. (C) 2009 Elsevier B.V. All rights reserved.
文献类型	期刊论文
条目标识符	http://ir.isl.ac.cn/handle/363002/1924
专题	青海盐湖研究所知识仓储
推荐引用方式 GB/T 7714	Long, Hao,Lai, ZhongPing,Fan, QiShun,et al. Applicability of a quartz OSL standardised growth curve for D-edetermination up to 400 Gy for lacustrine sediments from the QaidamBasin of the Qinghai-Tibetan Plateau[J]. QUATERNARY GEOCHRONOLOGY,2010,5(2-3):212-217.
APA	Long, Hao,Lai, ZhongPing,Fan, QiShun,Sun, YongJuan,&Liu, XiangJun.(2010).Applicability of a quartz OSL standardised growth curve for D-edetermination up to 400 Gy for lacustrine sediments from the QaidamBasin of the Qinghai-Tibetan Plateau.QUATERNARY GEOCHRONOLOGY,5(2-3),212-217.
MLA	Long, Hao,et al."Applicability of a quartz OSL standardised growth curve for D-edetermination up to 400 Gy for lacustrine sediments from the QaidamBasin of the Qinghai-Tibetan Plateau".QUATERNARY GEOCHRONOLOGY 5.2-3(2010):212-217.