唐古拉山东段布加岗日南坡小冰期冰进的10Be暴露测年研究
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赵井东, 邱锦坤, 季卉晗, 郭万钦, 刘瑞连, 麻浩男
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10Be surface exposure dating of Little Ice Age glacial events on the southern slope of Bujia Gangri, eastern Tanggula Mountains
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Jingdong ZHAO, Jinkun QIU, Huihan JI, Wanqin GUO, Ruilian LIU, Haonan MA
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图5 青藏高原及周边山地新近获得LIA测年结果的研究参阅点 注:①唐古拉山东段布加岗日南坡(本文)、②喜马拉雅山卡若拉垭口地区[5]、③不丹喜马拉雅山北坡Cogarbu流域[6]、④不丹喜马拉雅山北坡Shimo冰川区[7]、⑤冈底斯山脉的申扎杰岗日地区[8]、⑥冈底斯山冷布岗日地区[9]、⑦印度北部Garhwal中部山区[10]、⑧喜马拉雅—西藏造山带西北端Hamtah和Karzok流域[11]、⑨印度西北部Kulti与Parkachik流域[12]、⑩印度西北部Nun-Kun山区[13]、? 天山那拉提山地区[35]、? 天山乌鲁木齐河源区与哈希勒根达坂[36]、? 天山乌鲁木齐河源区[37]、? 天山哈尔里克山地区[38]、? 贡嘎山海螺沟[19]。红线为季风与非季风区分界线[39]
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Fig. 5 LIA glacial advance dated by 10Be dating techniques recently on the Tibetan Plateau and its surroundings Note: ① This study; ② Karola Pass area, the Himalayas[5]; ③ Cogarbu valley, Bhutanese Himalaya[6]; ④ Shimo Glacier valley, Bhutanese Himalaya[7]; ⑤ Mount Jaggang area, Gangdise Mountains[8]; ⑥ Lopu Kangri area, Gangdise Mountains[9]; ⑦ Central Garhwal Mountains, northern India[10]; ⑧ Hamtah and Karzok valleys at the northwestern end of the Himalayan-Tibetan orogen[11]; ⑨ Kulti and Parkachik valleys, northwestern India[12]; ⑩Nun-Kun mountainous area, northwestern India[13]; ? Nalati Mountains, Tianshan range[35]; ? Headwater of the Urumqi River and Haxilegen Pass area, Tianshan range[36]; ? Headwater of the Urumqi River, Tianshan range[37]; ? Karlik Mountain, Tianshan range[38]; ? Hailuogou valley, Mount Gongga[19]. Red line is the boundary of modern summer monsoon[39]
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