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	New evidence for enhanced cosmogenic isotope production rate in the atmosphere similar to 37 ka BP
	Wang, NL; Yao, TD; Qin, DH; Thompson, LG; Mosley-Thompson, E; Cole-Dai, J; Davis, ME; Lin, PN
发表日期	1999
ISSN	0260-3055
起始页码	136
结束页码	140
卷号	29
英文摘要	A Cl-36 peak has been found at about 37 ka np in the Guliya ice core, drilled from the Qinghai-Tibetan Plateau. This peak is indicative of enhanced cosmogenic isotope production in the atmosphere, rather than a change in accumulation rate. Comparison with the records of Be-10 and Cl-36 in ice cores from Antarctica and Greenland indicates that peaks of the cosmogenic isotopes are global, and that they can be used as time markers for dating ice cores. Interestingly, the 37 ka sp global event coincided with a cold period.
WOS研究方向	Geochemistry & Geophysics ; Physical Geography
WOS类目	Geochemistry & Geophysics ; Geography, Physical
来源期刊	ANNALS OF GLACIOLOGY, VOL 29, 1999
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/158773
作者单位	Wang, NL (corresponding author), Chinese Acad Sci, Lanzhou Inst Glaciol & Geocryol, Lab Ice Core & Cold Reg Environm, Lanzhou 730000, Gansu, Peoples R China.
推荐引用方式 GB/T 7714	Wang, NL,Yao, TD,Qin, DH,et al. New evidence for enhanced cosmogenic isotope production rate in the atmosphere similar to 37 ka BP[J],1999,29.
APA	Wang, NL.,Yao, TD.,Qin, DH.,Thompson, LG.,Mosley-Thompson, E.,...&Lin, PN.(1999).New evidence for enhanced cosmogenic isotope production rate in the atmosphere similar to 37 ka BP.ANNALS OF GLACIOLOGY, VOL 29, 1999,29.
MLA	Wang, NL,et al."New evidence for enhanced cosmogenic isotope production rate in the atmosphere similar to 37 ka BP".ANNALS OF GLACIOLOGY, VOL 29, 1999 29(1999).