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DOI | 10.2478/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
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ISSN | 2081-9900 |
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 |
推荐引用方式 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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