Seasonal variability in the origin of recent atmospheric mineral dust at NorthGRIP, Greenland

被引：186

作者：

Bory, AJM ^{[1
]}

Biscaye, PE

Svensson, A

Grousset, FE

机构：

[1] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA

[2] Univ Copenhagen, Niels Bohr Inst Astron Phys & Geophys, DK-2100 Copenhagen O, Denmark

[3] Univ Bordeaux 1, Dept Geol & Oceanog, F-33405 Talence, France

来源：

EARTH AND PLANETARY SCIENCE LETTERS | 2002年 / 196卷 / 3-4期

基金：

美国国家科学基金会;

关键词：

dust; Greenland; GRIP; snow; mineralogy; Neodymium; strontium; Far East;

D O I：

10.1016/S0012-821X(01)00609-4

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Isotopic (Sr and Nd) and mineralogical analyses of dust extracted from snow deposits from the last decade at the NorthGRIP, Greenland, ice camp (75.1degreesN, 042.3degreesW) confirm the eastern Asian source for Greenland dust and extend it to the present day. The 1998 and 1999 samples, which represent a similar to2.4 month resolution of dust deposition, show that there are at least two east Asian sources for the Greenland dust that vary seasonally. The provenance of dust during the major, spring/summer deposition is the Takla Makan desert of northwest China. (C) 2002 Elsevier Science B.V. All rights reserved.

引用

页码：123 / 134

页数：12

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