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Behaviour of rare earth elements during submarine weathering of tholeiitic basalt
DREDGED oceanic basalts and those sampled by deep-ocean drilling have commonly undergone some weathering with subsequent changes in their chemical composition 1–7 . The rare-earth elements (REE) La–Lu are generally considered to be unaffected by weathering and are thus often used to characterise var...
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Published in: | Nature (London) 1978-07, Vol.274 (5667), p.147-149 |
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creator | LUDDEN, JOHN N THOMPSON, GEOFFREY |
description | DREDGED oceanic basalts and those sampled by deep-ocean drilling have commonly undergone some weathering with subsequent changes in their chemical composition
1–7
. The rare-earth elements (REE) La–Lu are generally considered to be unaffected by weathering and are thus often used to characterise variations in basalt and magma composition. When considered relative to chondritic abundances
8
, the overall REE distribution is a critical diagnostic tool. In particular, the relative depletion of light-REE is used to discriminate between magma types. We present here new findings which show that REE are affected by low-temperature weathering processes. In particular, the light-REE show enrichments which may result in a basalt with a primary light-REE depleted pattern showing a flat or enriched light-REE pattern. |
doi_str_mv | 10.1038/274147a0 |
format | article |
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1–7
. The rare-earth elements (REE) La–Lu are generally considered to be unaffected by weathering and are thus often used to characterise variations in basalt and magma composition. When considered relative to chondritic abundances
8
, the overall REE distribution is a critical diagnostic tool. In particular, the relative depletion of light-REE is used to discriminate between magma types. We present here new findings which show that REE are affected by low-temperature weathering processes. In particular, the light-REE show enrichments which may result in a basalt with a primary light-REE depleted pattern showing a flat or enriched light-REE pattern.</description><identifier>ISSN: 0028-0836</identifier><identifier>EISSN: 1476-4687</identifier><identifier>DOI: 10.1038/274147a0</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>Humanities and Social Sciences ; letter ; multidisciplinary ; Science ; Science (multidisciplinary)</subject><ispartof>Nature (London), 1978-07, Vol.274 (5667), p.147-149</ispartof><rights>Springer Nature Limited 1978</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a305t-d4d3a6917914e0c48999392762a24d3e29475de553f13f7d649d667f707aba4c3</citedby><cites>FETCH-LOGICAL-a305t-d4d3a6917914e0c48999392762a24d3e29475de553f13f7d649d667f707aba4c3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,2727,27924,27925</link.rule.ids></links><search><creatorcontrib>LUDDEN, JOHN N</creatorcontrib><creatorcontrib>THOMPSON, GEOFFREY</creatorcontrib><title>Behaviour of rare earth elements during submarine weathering of tholeiitic basalt</title><title>Nature (London)</title><addtitle>Nature</addtitle><description>DREDGED oceanic basalts and those sampled by deep-ocean drilling have commonly undergone some weathering with subsequent changes in their chemical composition
1–7
. The rare-earth elements (REE) La–Lu are generally considered to be unaffected by weathering and are thus often used to characterise variations in basalt and magma composition. When considered relative to chondritic abundances
8
, the overall REE distribution is a critical diagnostic tool. In particular, the relative depletion of light-REE is used to discriminate between magma types. We present here new findings which show that REE are affected by low-temperature weathering processes. In particular, the light-REE show enrichments which may result in a basalt with a primary light-REE depleted pattern showing a flat or enriched light-REE pattern.</description><subject>Humanities and Social Sciences</subject><subject>letter</subject><subject>multidisciplinary</subject><subject>Science</subject><subject>Science (multidisciplinary)</subject><issn>0028-0836</issn><issn>1476-4687</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1978</creationdate><recordtype>article</recordtype><recordid>eNptkE9PwzAMxSMEEmMg8QlQjnAoOE2aNEeYxh9pEkKCc-W1Lu3UtVOSgvj2ZAx24vQs-2fr-TF2LuBagMxvUqOEMggHbBJVJ0rn5pBNANI8gVzqY3bi_QoAMmHUhL3cUYMf7TA6PtTcoSNO6ELDqaM19cHzanRt_879uFxjrIh_EoaGfppxJTRDR20b2pIv0WMXTtlRjZ2ns1-dsrf7-evsMVk8PzzNbhcJSshCUqlKorbCWKEISpVba6VNjU4xjSNKrTJZRVkmayFrU2llK61NbcDgElUpp-xyd7d0g_eO6mLj2mjxqxBQbKMo_qKI6NUO9ZutbXLFKj7cR3f_sRc7tscwOtof3QPfvahoFg</recordid><startdate>19780713</startdate><enddate>19780713</enddate><creator>LUDDEN, JOHN N</creator><creator>THOMPSON, GEOFFREY</creator><general>Nature Publishing Group UK</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>19780713</creationdate><title>Behaviour of rare earth elements during submarine weathering of tholeiitic basalt</title><author>LUDDEN, JOHN N ; THOMPSON, GEOFFREY</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a305t-d4d3a6917914e0c48999392762a24d3e29475de553f13f7d649d667f707aba4c3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1978</creationdate><topic>Humanities and Social Sciences</topic><topic>letter</topic><topic>multidisciplinary</topic><topic>Science</topic><topic>Science (multidisciplinary)</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>LUDDEN, JOHN N</creatorcontrib><creatorcontrib>THOMPSON, GEOFFREY</creatorcontrib><collection>CrossRef</collection><jtitle>Nature (London)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>LUDDEN, JOHN N</au><au>THOMPSON, GEOFFREY</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Behaviour of rare earth elements during submarine weathering of tholeiitic basalt</atitle><jtitle>Nature (London)</jtitle><stitle>Nature</stitle><date>1978-07-13</date><risdate>1978</risdate><volume>274</volume><issue>5667</issue><spage>147</spage><epage>149</epage><pages>147-149</pages><issn>0028-0836</issn><eissn>1476-4687</eissn><abstract>DREDGED oceanic basalts and those sampled by deep-ocean drilling have commonly undergone some weathering with subsequent changes in their chemical composition
1–7
. The rare-earth elements (REE) La–Lu are generally considered to be unaffected by weathering and are thus often used to characterise variations in basalt and magma composition. When considered relative to chondritic abundances
8
, the overall REE distribution is a critical diagnostic tool. In particular, the relative depletion of light-REE is used to discriminate between magma types. We present here new findings which show that REE are affected by low-temperature weathering processes. In particular, the light-REE show enrichments which may result in a basalt with a primary light-REE depleted pattern showing a flat or enriched light-REE pattern.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><doi>10.1038/274147a0</doi><tpages>3</tpages></addata></record> |
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subjects | Humanities and Social Sciences letter multidisciplinary Science Science (multidisciplinary) |
title | Behaviour of rare earth elements during submarine weathering of tholeiitic basalt |
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