Morphoscopy and Morphometry of Quartz Grains from Loess and Buried Soil Layers
A complex method is suggested for the study of surfaces of sand grains. With this method, middle-and late Pleistocene loess-palaeosol sequences of the Russian Plain, Dnieper Basin, were studied. Surface texture of grains pointed to a dry and cold climate for their formation. During deposition of loe...
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Veröffentlicht in: | GeoJournal 1995-06, Vol.36 (2/3), p.143-149 |
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creator | Velichko, Andrej A. Timireva, Svetlana N. |
description | A complex method is suggested for the study of surfaces of sand grains. With this method, middle-and late Pleistocene loess-palaeosol sequences of the Russian Plain, Dnieper Basin, were studied. Surface texture of grains pointed to a dry and cold climate for their formation. During deposition of loess layers predominantly aeolian and cryogenic processes formed the grain surfaces. During interglacial and interstadial periods chemical weathering dominated. |
doi_str_mv | 10.1007/BF00813159 |
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With this method, middle-and late Pleistocene loess-palaeosol sequences of the Russian Plain, Dnieper Basin, were studied. Surface texture of grains pointed to a dry and cold climate for their formation. During deposition of loess layers predominantly aeolian and cryogenic processes formed the grain surfaces. 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With this method, middle-and late Pleistocene loess-palaeosol sequences of the Russian Plain, Dnieper Basin, were studied. Surface texture of grains pointed to a dry and cold climate for their formation. During deposition of loess layers predominantly aeolian and cryogenic processes formed the grain surfaces. During interglacial and interstadial periods chemical weathering dominated.</description><subject>Forest soils</subject><subject>Granulometrical and Morphoscopical Methods</subject><subject>Loess</subject><subject>Loess soils</subject><subject>Paleoecology</subject><subject>Paleogeography</subject><subject>Quartz</subject><subject>Russia</subject><subject>Sand</subject><subject>Sedimentary soils</subject><subject>Sediments</subject><subject>Soil chemistry</subject><subject>Soil horizons</subject><subject>Soils</subject><subject>Surface texture</subject><issn>0343-2521</issn><issn>1572-9893</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1995</creationdate><recordtype>article</recordtype><recordid>eNqF0EFLxDAQBeAgCq6rF-9CTh6E6kyTtM3RXdxVqIqo55JNE-zSbmrSHuqvt1rRo6eZgY-B9wg5RbhEgPRqsQLIkKGQe2SGIo0jmUm2T2bAOItiEeMhOQphCwAyTXFGHu6db99c0K4dqNqVdLob0_mBOkufeuW7D7r2qtoFar1raO5MCN920fvKlPTZVTXN1WB8OCYHVtXBnPzMOXld3bwsb6P8cX23vM4jFQvsIsbLWJbjngimtQQtTcLAMmM5t0rhhieZ3ABXEmKdidKkmVXI1BhOltZINifn09_Wu_fehK5oqqBNXaudcX0oWDamk0n8L8QMU-CCjfBigtq7ELyxReurRvmhQCi-ui3-uh3x2YS3oXP-V3JEnnAp2CdBYHS7</recordid><startdate>199506</startdate><enddate>199506</enddate><creator>Velichko, Andrej A.</creator><creator>Timireva, Svetlana N.</creator><general>Kluwer Academic Publishers</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>8BJ</scope><scope>FQK</scope><scope>JBE</scope></search><sort><creationdate>199506</creationdate><title>Morphoscopy and Morphometry of Quartz Grains from Loess and Buried Soil Layers</title><author>Velichko, Andrej A. ; Timireva, Svetlana N.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a251t-34d29da25653cc90c9e630f3ef44faa1b4689b04a902c85de78fa13a0089dfe93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1995</creationdate><topic>Forest soils</topic><topic>Granulometrical and Morphoscopical Methods</topic><topic>Loess</topic><topic>Loess soils</topic><topic>Paleoecology</topic><topic>Paleogeography</topic><topic>Quartz</topic><topic>Russia</topic><topic>Sand</topic><topic>Sedimentary soils</topic><topic>Sediments</topic><topic>Soil chemistry</topic><topic>Soil horizons</topic><topic>Soils</topic><topic>Surface texture</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Velichko, Andrej A.</creatorcontrib><creatorcontrib>Timireva, Svetlana N.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>International Bibliography of the Social Sciences (IBSS)</collection><collection>International Bibliography of the Social Sciences</collection><collection>International Bibliography of the Social Sciences</collection><jtitle>GeoJournal</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Velichko, Andrej A.</au><au>Timireva, Svetlana N.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Morphoscopy and Morphometry of Quartz Grains from Loess and Buried Soil Layers</atitle><jtitle>GeoJournal</jtitle><date>1995-06</date><risdate>1995</risdate><volume>36</volume><issue>2/3</issue><spage>143</spage><epage>149</epage><pages>143-149</pages><issn>0343-2521</issn><eissn>1572-9893</eissn><abstract>A complex method is suggested for the study of surfaces of sand grains. With this method, middle-and late Pleistocene loess-palaeosol sequences of the Russian Plain, Dnieper Basin, were studied. Surface texture of grains pointed to a dry and cold climate for their formation. During deposition of loess layers predominantly aeolian and cryogenic processes formed the grain surfaces. During interglacial and interstadial periods chemical weathering dominated.</abstract><pub>Kluwer Academic Publishers</pub><doi>10.1007/BF00813159</doi><tpages>7</tpages></addata></record> |
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subjects | Forest soils Granulometrical and Morphoscopical Methods Loess Loess soils Paleoecology Paleogeography Quartz Russia Sand Sedimentary soils Sediments Soil chemistry Soil horizons Soils Surface texture |
title | Morphoscopy and Morphometry of Quartz Grains from Loess and Buried Soil Layers |
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