首页|青藏高原腹地各拉丹冬峰东坡现代冰川地形10Be暴露测年的初步研究

青藏高原腹地各拉丹冬峰东坡现代冰川地形10Be暴露测年的初步研究

扫码查看
青藏高原及周边山地现代冰川外围新鲜无风化的冰川地形多为小冰期结束后冰川退缩所成,这些地形包含有近几十年至上百年的气候环境变化信息,对它们进行研究有望揭示101年时间尺度上的冰川波动并探讨其驱动机制。本文尝试应用原生宇宙成因核素10Be暴露测年技术对青藏高原腹地,唐古拉山西段各拉丹冬峰地区的岗加曲巴冰川外围的现代冰川地形进行年代测定。测得1969年冰川退缩后出露的基岩磨光面的年龄为(11076±688)a(G19-01);1969年至小冰期冰碛垄间底碛中5个花岗岩漂砾(G19-02~06)的年龄分别为(125±15)a、(65±13)a、(86±13)a、(96±15)a、(104±15)a。测年结果显示冰川磨光面的年龄与地貌关系明显不符,推测是基岩表层侵蚀量不足,未能有效去除先前累积的核素所致;漂砾的测年结果与地貌关系基本相吻合。本研究表明,在10Be产率较高的高原山地,若能采集到基本未受核素继承影响的漂砾,增加纯石英的使用量可测定近百年来所成的现代冰川地形的年龄。本文测得的10Be年龄进一步表明该测年技术具有细化101年时间尺度上冰川波动的潜在应用前景和弥补青藏高原腹地气候环境变化器测记录和代用指标的不足,对高海拔地区年轻地貌体的年代测定研究也有一定的借鉴意义。
10Be surface exposure dating of young glacial landforms on eastern slope of Mount Geladandong,central Qinghai-Xizang Plateau
The young glacial erosional and depositional landforms beyond the modern glaciers on the Qinghai-Xizang Plateau and its surroundings are direct imprints of the glacier fluctuation during the past several decades or century,and contain important palaeoclimatic and palaeoenvironmental information. Studies of these land-forms could provide insights into the spatiotemporal variations of these ancient glaciers. Improved logistics and the development and application of the terrestrial in situ cosmogenic nuclide (TCN) 10Be surface exposure dating techniques,are making it to be possible to investigate the young glacial landforms in the Mount Geladandong ar-ea,which locates in the west segment of the Tanggula Mountains,central Qinghai-Xizang Plateau. Here we re-port on 10Be surface exposure dating of six samples collected from modern glacial landforms associated with the Gangjiaquba Glacier on the eastern slope of Mount Geladandong. Dating results demonstrate that the boulders[samples from G19-02 to G19-06 and their ages are (125±15) a、(65±13) a、(86±13) a、(96±15) a、(104±15) a]were almost not affected by nuclide inheritance,and the 10Be surface exposure ages could be used to constrain glacier fluctuations during the past century in this high-altitude area. However,a comparison of the ages of a gla-cially polished surface[sample of G19-01 and its age is (11076±688) a]and boulders indicates that subglacial erosion by abrasion of the rock surface was insufficient (<2 m) to remove cosmogenic nuclide inventories. Thus,the apparent exposure age on the polished surface includes inheritance and overestimates the true age of this surface. Our study suggests that a cautious sampling and interpretation strategy should be adopted with bed-rock samples,and the 10Be surface exposure dating techniques have potential applications for dating glacier fluc-tuations on a 101-year time scale in these high-altitude areas with high 10Be production rates. Meanwhile,this study also provides a new reference for the application of 10Be exposure dating technique in dating the young land-forms in high altitude areas.

10Be surface exposure datingmodern glacial landformsTanggula Mountainscentral Qinghai-Xizang Plateau

陈净玲、赵井东、邱锦坤、季卉晗、郭万钦、刘瑞连、何晓波

展开 >

中国科学院西北生态环境资源研究院冰冻圈科学国家重点实验室,甘肃兰州 730000

中国科学院大学,北京 100049

兰州大学资源环境学院 西部环境教育部重点实验室,甘肃兰州 730000

唐古拉山冰冻圈与环境西藏自治区野外科学观测研究站,甘肃兰州 730000

展开 >

10Be暴露测年 现代冰川地形 唐古拉山 青藏高原腹地

国家自然科学基金项目国家自然科学基金项目国家自然科学基金项目第二次青藏高原综合科学考察研究

4177101841830644422711562019QZKK0201

2024

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCD
影响因子:2.546
ISSN:1000-0240
年,卷(期):2024.46(4)