Secondary alteration in eclogites from kimberlite pipes

An analcime-type zeolite has been found in eclogite xenoliths from a kimberlite pipe. Analytical data obtained for the primary pyroxene (omphacite) and secondary minerals (mica, analcime, clay) indicate that the xenoliths have been contaminated by K,Rb and Cs, which are important for the study of th...

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Veröffentlicht in:The American mineralogist 1968-08, Vol.53 (7-8), p.1336-1346
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description An analcime-type zeolite has been found in eclogite xenoliths from a kimberlite pipe. Analytical data obtained for the primary pyroxene (omphacite) and secondary minerals (mica, analcime, clay) indicate that the xenoliths have been contaminated by K,Rb and Cs, which are important for the study of the origin of eclogites. Metasomatic alteration of an eclogite during the intrusion of the kimberlite may be followed by further contamination of the eclogite by the migration of elements during the weathering of the kimberlite. For many elements abundance data must be determined on separated primary eclogite minerals and data obtained on whole-rocks should be treated with some circumspection.
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W</creator><creatorcontrib>Berg, G. W</creatorcontrib><description>An analcime-type zeolite has been found in eclogite xenoliths from a kimberlite pipe. Analytical data obtained for the primary pyroxene (omphacite) and secondary minerals (mica, analcime, clay) indicate that the xenoliths have been contaminated by K,Rb and Cs, which are important for the study of the origin of eclogites. Metasomatic alteration of an eclogite during the intrusion of the kimberlite may be followed by further contamination of the eclogite by the migration of elements during the weathering of the kimberlite. For many elements abundance data must be determined on separated primary eclogite minerals and data obtained on whole-rocks should be treated with some circumspection.</description><identifier>ISSN: 0003-004X</identifier><identifier>EISSN: 1945-3027</identifier><language>eng</language><publisher>Mineralogical Society of America</publisher><subject>Africa ; alteration ; Alteration products of eclogites ; eclogite ; framework silicates ; igneous rocks ; kimberlite ; kimberlite pipes ; major-element analyses ; metamorphic rocks ; mineral data ; mineralogy ; Roberts Victor mine ; secondary ; silicates ; South Africa ; Southern Africa ; ultramafic composition ; weathering ; zeolite ; zeolite alteration ; zeolite group ; zeolites</subject><ispartof>The American mineralogist, 1968-08, Vol.53 (7-8), p.1336-1346</ispartof><rights>GeoRef, Copyright 2020, American Geosciences Institute. Reference includes data from Bibliography and Index of North American Geology, U. S. 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Metasomatic alteration of an eclogite during the intrusion of the kimberlite may be followed by further contamination of the eclogite by the migration of elements during the weathering of the kimberlite. For many elements abundance data must be determined on separated primary eclogite minerals and data obtained on whole-rocks should be treated with some circumspection.</description><subject>Africa</subject><subject>alteration</subject><subject>Alteration products of eclogites</subject><subject>eclogite</subject><subject>framework silicates</subject><subject>igneous rocks</subject><subject>kimberlite</subject><subject>kimberlite pipes</subject><subject>major-element analyses</subject><subject>metamorphic rocks</subject><subject>mineral data</subject><subject>mineralogy</subject><subject>Roberts Victor mine</subject><subject>secondary</subject><subject>silicates</subject><subject>South Africa</subject><subject>Southern Africa</subject><subject>ultramafic composition</subject><subject>weathering</subject><subject>zeolite</subject><subject>zeolite alteration</subject><subject>zeolite group</subject><subject>zeolites</subject><issn>0003-004X</issn><issn>1945-3027</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1968</creationdate><recordtype>article</recordtype><sourceid/><recordid>eNotj0tLxDAUhYMoWEf_Q_YSuHncplnK4AsGXKjgrqTN7ZCxkwxJRfz3FnR14HD4Ps4Za6QzKDQoe84aANACwHxcsqtaDwBKaXQNs6805hR8-eF-Xqj4JebEY-I0znkfF6p8KvnIP-NxoDKvBT_FE9VrdjH5udLNf27Y-8P92_ZJ7F4en7d3O-GlMYtYHVa1GkzrlEILU2fNNAVyMshAUiGqoAIaQEAkonWBrpVDcNT5QWm9Ybd_3D3lOkZKI33nMof-kL9KWs29dG3XAzqzPvwFMy5FkA</recordid><startdate>196808</startdate><enddate>196808</enddate><creator>Berg, G. 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Metasomatic alteration of an eclogite during the intrusion of the kimberlite may be followed by further contamination of the eclogite by the migration of elements during the weathering of the kimberlite. For many elements abundance data must be determined on separated primary eclogite minerals and data obtained on whole-rocks should be treated with some circumspection.</abstract><pub>Mineralogical Society of America</pub><tpages>11</tpages></addata></record>
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subjects Africa
alteration
Alteration products of eclogites
eclogite
framework silicates
igneous rocks
kimberlite
kimberlite pipes
major-element analyses
metamorphic rocks
mineral data
mineralogy
Roberts Victor mine
secondary
silicates
South Africa
Southern Africa
ultramafic composition
weathering
zeolite
zeolite alteration
zeolite group
zeolites
title Secondary alteration in eclogites from kimberlite pipes
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