Arid
DOI10.2478/v10085-010-0034-3
A size control for quartz silt (making particulates at planetary surfaces)
Smalley, Ian1; Vita-Finzi, Claudio2
通讯作者Smalley, Ian
来源期刊CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES
ISSN2081-9900
出版年2011
卷号3期号:1页码:37-38
英文摘要

Quartz silt is widespread in terrestrial sediments [1]. Its ubiquity has led to its neglect as a geomaterial, and studies of silt as such are relatively rare, but it presents an interesting and continuing petrological problem. Is silt a specific geological material, is it defined by a formation process, and a set of size parameters? In the world of clastic quartz sedimentology there are obvious mode sizes; there is a sand mode at around 300-500 mu m and a silt mode, an order of magnitude smaller, at 30-50 mu m. Are these both defined by specific geological processes?


英文关键词quartz silt formation mechanism Mars sediments
类型Editorial Material
语种英语
国家England
收录类别SCI-E
WOS记录号WOS:000307253300004
WOS关键词DESERT LOESS ; SAND SEAS
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/167553
作者单位1.Nottingham Trent Univ, Giotto Loess Res Grp, Arkwright Mat Project, Nottingham NG1 4BU, England;
2.Nat Hist Museum, Dept Mineral, London SW7 5BD, England
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GB/T 7714
Smalley, Ian,Vita-Finzi, Claudio. A size control for quartz silt (making particulates at planetary surfaces)[J],2011,3(1):37-38.
APA Smalley, Ian,&Vita-Finzi, Claudio.(2011).A size control for quartz silt (making particulates at planetary surfaces).CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES,3(1),37-38.
MLA Smalley, Ian,et al."A size control for quartz silt (making particulates at planetary surfaces)".CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES 3.1(2011):37-38.
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