The Tertiary to Recent North Atlantic igneous

An occurrence of basic pillows enclosed in a syenitic matrix is described from the little-known Kialineq district. Cuspate margins, chilled contacts and long fingers of syenite extending upwards into the basic material are evidence that the two magmas were fluid at the same time. Hybridization betwe...

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Main Author: C. K. Brooks
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.1935
http://2dgf.dk/xpdf/bull26-01-02-77-83.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.520.1935 2023-05-15T16:03:40+02:00 The Tertiary to Recent North Atlantic igneous C. K. Brooks The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.1935 http://2dgf.dk/xpdf/bull26-01-02-77-83.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.1935 http://2dgf.dk/xpdf/bull26-01-02-77-83.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://2dgf.dk/xpdf/bull26-01-02-77-83.pdf text ftciteseerx 2016-01-08T10:05:27Z An occurrence of basic pillows enclosed in a syenitic matrix is described from the little-known Kialineq district. Cuspate margins, chilled contacts and long fingers of syenite extending upwards into the basic material are evidence that the two magmas were fluid at the same time. Hybridization between these two magmas has produced a microdiorite. The chemical variation in these rocks is linear and quite dissimilar to that observed in other suites from the East Greenland Tertiary but resembles that observed both in mixed rocks from other parts of the province, e.g. eastern Iceland, and in calc-alkaline rocks from orogenic regions. Text East Greenland Greenland Iceland North Atlantic Unknown Greenland Kialineq ENVELOPE(-33.783,-33.783,66.933,66.933)
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description An occurrence of basic pillows enclosed in a syenitic matrix is described from the little-known Kialineq district. Cuspate margins, chilled contacts and long fingers of syenite extending upwards into the basic material are evidence that the two magmas were fluid at the same time. Hybridization between these two magmas has produced a microdiorite. The chemical variation in these rocks is linear and quite dissimilar to that observed in other suites from the East Greenland Tertiary but resembles that observed both in mixed rocks from other parts of the province, e.g. eastern Iceland, and in calc-alkaline rocks from orogenic regions.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author C. K. Brooks
spellingShingle C. K. Brooks
The Tertiary to Recent North Atlantic igneous
author_facet C. K. Brooks
author_sort C. K. Brooks
title The Tertiary to Recent North Atlantic igneous
title_short The Tertiary to Recent North Atlantic igneous
title_full The Tertiary to Recent North Atlantic igneous
title_fullStr The Tertiary to Recent North Atlantic igneous
title_full_unstemmed The Tertiary to Recent North Atlantic igneous
title_sort tertiary to recent north atlantic igneous
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.520.1935
http://2dgf.dk/xpdf/bull26-01-02-77-83.pdf
long_lat ENVELOPE(-33.783,-33.783,66.933,66.933)
geographic Greenland
Kialineq
geographic_facet Greenland
Kialineq
genre East Greenland
Greenland
Iceland
North Atlantic
genre_facet East Greenland
Greenland
Iceland
North Atlantic
op_source http://2dgf.dk/xpdf/bull26-01-02-77-83.pdf
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http://2dgf.dk/xpdf/bull26-01-02-77-83.pdf
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