Origin and Mineralogy Glacial and Interglacial Clays of Southern Norway
The Numedal River basin (6000 km 2 ) in central and east Norway contains 3 × 10 9 m 3 of clayey material, corresponding to a clay loam sediment, which contains 2 million tons of absorbed rare earth elements. The clay mineralogy varies systematically from the till clays to a marine facies. It is conc...
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| Veröffentlicht in: | Clays and clay minerals 1975-04, Vol.23 (2), p.153-159 |
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| container_title | Clays and clay minerals |
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| creator | Rosenqvist, I. Th |
| description | The Numedal River basin (6000 km 2 ) in central and east Norway contains 3 × 10 9 m 3 of clayey material, corresponding to a clay loam sediment, which contains 2 million tons of absorbed rare earth elements.
The clay mineralogy varies systematically from the till clays to a marine facies. It is concluded that the phyllosilicates of the clay fraction and tills originated from phyllosilicate minerals of the crystalline bedrock through a degradation partly due to preQuaternary weathering which dissolved a great part of the rock-forming minerals. |
| doi_str_mv | 10.1346/CCMN.1975.0230211 |
| format | Article |
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The clay mineralogy varies systematically from the till clays to a marine facies. It is concluded that the phyllosilicates of the clay fraction and tills originated from phyllosilicate minerals of the crystalline bedrock through a degradation partly due to preQuaternary weathering which dissolved a great part of the rock-forming minerals.</description><identifier>ISSN: 0009-8604</identifier><identifier>EISSN: 1552-8367</identifier><identifier>DOI: 10.1346/CCMN.1975.0230211</identifier><language>eng</language><ispartof>Clays and clay minerals, 1975-04, Vol.23 (2), p.153-159</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a332t-f936224b5044ec622bbb2b38c201bddfed1585316ddb774792f2b5f1132b0a903</citedby><cites>FETCH-LOGICAL-a332t-f936224b5044ec622bbb2b38c201bddfed1585316ddb774792f2b5f1132b0a903</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Rosenqvist, I. Th</creatorcontrib><title>Origin and Mineralogy Glacial and Interglacial Clays of Southern Norway</title><title>Clays and clay minerals</title><description>The Numedal River basin (6000 km 2 ) in central and east Norway contains 3 × 10 9 m 3 of clayey material, corresponding to a clay loam sediment, which contains 2 million tons of absorbed rare earth elements.
The clay mineralogy varies systematically from the till clays to a marine facies. It is concluded that the phyllosilicates of the clay fraction and tills originated from phyllosilicate minerals of the crystalline bedrock through a degradation partly due to preQuaternary weathering which dissolved a great part of the rock-forming minerals.</description><issn>0009-8604</issn><issn>1552-8367</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1975</creationdate><recordtype>article</recordtype><recordid>eNot0M1OhDAUBeDGaCKOPoA7XgC89_YHWBqi4yTzs1DXpKUtYhBMwRjeXlFW5-QszuJj7BYhRS7UXVkejikWmUyBOBDiGYtQSkpyrrJzFgFAkeQKxCW7Gsd3AFKCU8S2p9A2bR_r3saHtndBd0Mzx9tO163u_uZdP7nQrEPZ6XmMBx8_D1_Tmwt9fBzCt56v2YXX3ehu1tyw18eHl_Ip2Z-2u_J-n2jOaUp8wRWRMBKEcPVvNcaQ4XlNgMZa7yzKXHJU1posE1lBnoz0iJwM6AL4huH_bx2GcQzOV5-h_dBhrhCqRaJaJKpFolol-A-sYlDI</recordid><startdate>197504</startdate><enddate>197504</enddate><creator>Rosenqvist, I. Th</creator><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>197504</creationdate><title>Origin and Mineralogy Glacial and Interglacial Clays of Southern Norway</title><author>Rosenqvist, I. Th</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a332t-f936224b5044ec622bbb2b38c201bddfed1585316ddb774792f2b5f1132b0a903</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1975</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Rosenqvist, I. Th</creatorcontrib><collection>CrossRef</collection><jtitle>Clays and clay minerals</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Rosenqvist, I. Th</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Origin and Mineralogy Glacial and Interglacial Clays of Southern Norway</atitle><jtitle>Clays and clay minerals</jtitle><date>1975-04</date><risdate>1975</risdate><volume>23</volume><issue>2</issue><spage>153</spage><epage>159</epage><pages>153-159</pages><issn>0009-8604</issn><eissn>1552-8367</eissn><abstract>The Numedal River basin (6000 km 2 ) in central and east Norway contains 3 × 10 9 m 3 of clayey material, corresponding to a clay loam sediment, which contains 2 million tons of absorbed rare earth elements.
The clay mineralogy varies systematically from the till clays to a marine facies. It is concluded that the phyllosilicates of the clay fraction and tills originated from phyllosilicate minerals of the crystalline bedrock through a degradation partly due to preQuaternary weathering which dissolved a great part of the rock-forming minerals.</abstract><doi>10.1346/CCMN.1975.0230211</doi><tpages>7</tpages></addata></record> |
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| title | Origin and Mineralogy Glacial and Interglacial Clays of Southern Norway |
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