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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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. |
_version_ |
1766150541410304000 |