Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.apgeochem.2019.05.006 |
The geochemistry of glacial deposits in Taylor Valley, Antarctica: Comparison to upper continental crustal abundances | |
Dowling, Carolyn B.1; Welch, Susan A.2,3; Lyons, W. Berry2,3 | |
通讯作者 | Welch, Susan A. |
来源期刊 | APPLIED GEOCHEMISTRY
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ISSN | 0883-2927 |
出版年 | 2019 |
卷号 | 107页码:91-104 |
英文摘要 | Wet-based glacial deposits have been used traditionally as an analog for upper continental crust (UCC) abundances. To provide more information on the validity of using glacial deposits from wet-based glaciers, samples deposited by the dry-based polar glaciers located in Taylor Valley, Antarctica, were collected. Stream channel sediments, comprised of igneous, metamorphic, and sedimentary rocks initially deposited as glacial tills by polar glaciers, were analyzed by XRF, ICP-MS, and SEM. Based on the Chemical Index of Alteration values and A-CN-K ternary diagram, there are low levels of chemical weathering in these tills. Additionally, major and trace element geochemical data are compared to the average UCC values. The observed discrepancies between the mean UCC and Antarctic samples develop from the existence of mafic components, most likely the McMurdo Volcanic Group and Ferrar Dolerite, being present in the Taylor Valley tills. Even though the mafic material typically comprises 3-7% of the till, the volcanic rocks have a significant influence on the till's bulk geochemistry. The existence of this mafic fraction in the dry-based glacial tills results from the reduced rate of weathering, as compared to wet-based glaciers. Geochemical analyses of the dry-based glacial tills in polar deserts, such as those found in Taylor Valley, may provide a better representative composition of the original material than wet-based glaciers and need to be incorporated into upper continental crust calculations. |
英文关键词 | polar dry-based glaciers Geochemistry Glacial deposits Taylor valley Antarctica |
类型 | Article |
语种 | 英语 |
国家 | USA |
收录类别 | SCI-E |
WOS记录号 | WOS:000476985500008 |
WOS关键词 | DRY VALLEYS ; ICE-SHEET ; ROSS SEA ; SILICICLASTIC SEDIMENTS ; EVOLUTION ; TRANSPORT ; STREAMS ; PETROGENESIS ; DENUDATION ; CHEMISTRY |
WOS类目 | Geochemistry & Geophysics |
WOS研究方向 | Geochemistry & Geophysics |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/214258 |
作者单位 | 1.Ball State Univ, Dept Geol Sci, 2000 West Univ Ave, Muncie, IN 47306 USA; 2.Ohio State Univ, Sch Earth Sci, 125 South Oval Mall, Columbus, OH 43210 USA; 3.Ohio State Univ, Byrd Polar & Climate Res Ctr, 108 Scott Hall, Columbus, OH 43210 USA |
推荐引用方式 GB/T 7714 | Dowling, Carolyn B.,Welch, Susan A.,Lyons, W. Berry. The geochemistry of glacial deposits in Taylor Valley, Antarctica: Comparison to upper continental crustal abundances[J],2019,107:91-104. |
APA | Dowling, Carolyn B.,Welch, Susan A.,&Lyons, W. Berry.(2019).The geochemistry of glacial deposits in Taylor Valley, Antarctica: Comparison to upper continental crustal abundances.APPLIED GEOCHEMISTRY,107,91-104. |
MLA | Dowling, Carolyn B.,et al."The geochemistry of glacial deposits in Taylor Valley, Antarctica: Comparison to upper continental crustal abundances".APPLIED GEOCHEMISTRY 107(2019):91-104. |
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