A CASE STUDY OF THE EVOLUTION OF THE ELBAITE SUBTYPE OF RARE-ELEMENT GRANITIC PEGMATITE

The first confirmed Canadian occurrence of the elbaite subtype of rare-element granitic pegmatite has been encountered within the O’Grady batholith, approximately 100 km NNW of Tungsten, N.W.T. The batholith, part of the Selwyn plutonic suite, is a mesozonal, hornblende-bearing, metaluminous composi...

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Main Authors: T. Scott Ercit, Lee A. Groat, Robert A. Gault
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.542.9999
http://rruff.info/doclib/cm/vol41/CM41_117.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.542.9999 2023-05-15T17:46:43+02:00 A CASE STUDY OF THE EVOLUTION OF THE ELBAITE SUBTYPE OF RARE-ELEMENT GRANITIC PEGMATITE T. Scott Ercit Lee A. Groat Robert A. Gault The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.542.9999 http://rruff.info/doclib/cm/vol41/CM41_117.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.542.9999 http://rruff.info/doclib/cm/vol41/CM41_117.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://rruff.info/doclib/cm/vol41/CM41_117.pdf granitic pegmatite elbaite subtype principal components analysis melt evolution accessory minerals O’Grady batholith Selwyn plutonic suite Northwest Territories. SOMMAIRE text ftciteseerx 2016-01-08T11:09:35Z The first confirmed Canadian occurrence of the elbaite subtype of rare-element granitic pegmatite has been encountered within the O’Grady batholith, approximately 100 km NNW of Tungsten, N.W.T. The batholith, part of the Selwyn plutonic suite, is a mesozonal, hornblende-bearing, metaluminous composite intrusion with lesser amounts of pegmatitic granite and felsitic satellite dykes. On the whole, pegmatite bodies show a mildly NYF-type geochemical and mineralogical signature (allanite- and magnetite-bearing), but in the region of the pegmatitic granite, they grade toward a distinct LCT-type signature (elbaite-bearing). The melts parental to the pegmatite bodies were more voluminous, more alkaline, less aluminous and less reduced than is the norm for melts parental to LCT-type pegmatite. Differentiation of these melts sequentially produced hornblende granite, pegmatitic leucogranite and pegmatite, as shown by major-, minor- and trace-element geochemistry of K-feldspar, plagioclase, micas, tourmaline, amphibole and a variety of accessory phases. Lithium-mineralized pegmatite is recognized by the presence of multicolored elbaite, by lepidolite, and in the diversity of characteristic accessory phases such as danburite, hambergite, stibiocolumbite, pollucite, a nanpingite-like mineral, and bismutite. The various stages of the evolution of the batholith can be well documented in similar variations in mineral chemistry, and result in one of the few well-characterized case studies of the Text Northwest Territories Unknown Northwest Territories Selwyn ENVELOPE(-138.287,-138.287,62.799,62.799)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic granitic pegmatite
elbaite subtype
principal components analysis
melt evolution
accessory minerals
O’Grady batholith
Selwyn plutonic suite
Northwest Territories. SOMMAIRE
spellingShingle granitic pegmatite
elbaite subtype
principal components analysis
melt evolution
accessory minerals
O’Grady batholith
Selwyn plutonic suite
Northwest Territories. SOMMAIRE
T. Scott Ercit
Lee A. Groat
Robert A. Gault
A CASE STUDY OF THE EVOLUTION OF THE ELBAITE SUBTYPE OF RARE-ELEMENT GRANITIC PEGMATITE
topic_facet granitic pegmatite
elbaite subtype
principal components analysis
melt evolution
accessory minerals
O’Grady batholith
Selwyn plutonic suite
Northwest Territories. SOMMAIRE
description The first confirmed Canadian occurrence of the elbaite subtype of rare-element granitic pegmatite has been encountered within the O’Grady batholith, approximately 100 km NNW of Tungsten, N.W.T. The batholith, part of the Selwyn plutonic suite, is a mesozonal, hornblende-bearing, metaluminous composite intrusion with lesser amounts of pegmatitic granite and felsitic satellite dykes. On the whole, pegmatite bodies show a mildly NYF-type geochemical and mineralogical signature (allanite- and magnetite-bearing), but in the region of the pegmatitic granite, they grade toward a distinct LCT-type signature (elbaite-bearing). The melts parental to the pegmatite bodies were more voluminous, more alkaline, less aluminous and less reduced than is the norm for melts parental to LCT-type pegmatite. Differentiation of these melts sequentially produced hornblende granite, pegmatitic leucogranite and pegmatite, as shown by major-, minor- and trace-element geochemistry of K-feldspar, plagioclase, micas, tourmaline, amphibole and a variety of accessory phases. Lithium-mineralized pegmatite is recognized by the presence of multicolored elbaite, by lepidolite, and in the diversity of characteristic accessory phases such as danburite, hambergite, stibiocolumbite, pollucite, a nanpingite-like mineral, and bismutite. The various stages of the evolution of the batholith can be well documented in similar variations in mineral chemistry, and result in one of the few well-characterized case studies of the
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author T. Scott Ercit
Lee A. Groat
Robert A. Gault
author_facet T. Scott Ercit
Lee A. Groat
Robert A. Gault
author_sort T. Scott Ercit
title A CASE STUDY OF THE EVOLUTION OF THE ELBAITE SUBTYPE OF RARE-ELEMENT GRANITIC PEGMATITE
title_short A CASE STUDY OF THE EVOLUTION OF THE ELBAITE SUBTYPE OF RARE-ELEMENT GRANITIC PEGMATITE
title_full A CASE STUDY OF THE EVOLUTION OF THE ELBAITE SUBTYPE OF RARE-ELEMENT GRANITIC PEGMATITE
title_fullStr A CASE STUDY OF THE EVOLUTION OF THE ELBAITE SUBTYPE OF RARE-ELEMENT GRANITIC PEGMATITE
title_full_unstemmed A CASE STUDY OF THE EVOLUTION OF THE ELBAITE SUBTYPE OF RARE-ELEMENT GRANITIC PEGMATITE
title_sort case study of the evolution of the elbaite subtype of rare-element granitic pegmatite
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.542.9999
http://rruff.info/doclib/cm/vol41/CM41_117.pdf
long_lat ENVELOPE(-138.287,-138.287,62.799,62.799)
geographic Northwest Territories
Selwyn
geographic_facet Northwest Territories
Selwyn
genre Northwest Territories
genre_facet Northwest Territories
op_source http://rruff.info/doclib/cm/vol41/CM41_117.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.542.9999
http://rruff.info/doclib/cm/vol41/CM41_117.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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