Geological Museum, Copenhagen

logically to the crystal class 7~2m. The paper describes pseudotrigonal contact riplets recently found as freely developed individuals on two specimens donated to the Geological Museum, Copenhagen. The contact triplets, described as a symmetric twin, have the composition planes, which are also the t...

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Main Authors: Ole V. Petersen, Space Group, Belongs Morpho
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=10.1.1.601.3505
http://www.minersoc.org/pages/Archive-MM/Volume_42/42-322-251.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.601.3505 2023-05-15T16:29:31+02:00 Geological Museum, Copenhagen Ole V. Petersen Space Group Belongs Morpho The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.601.3505 http://www.minersoc.org/pages/Archive-MM/Volume_42/42-322-251.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.601.3505 http://www.minersoc.org/pages/Archive-MM/Volume_42/42-322-251.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.minersoc.org/pages/Archive-MM/Volume_42/42-322-251.pdf text ftciteseerx 2016-01-08T14:03:14Z logically to the crystal class 7~2m. The paper describes pseudotrigonal contact riplets recently found as freely developed individuals on two specimens donated to the Geological Museum, Copenhagen. The contact triplets, described as a symmetric twin, have the composition planes, which are also the twin planes, (io0 and (o I i); the pseudo-threefold axis, along which the crystals are pronouncedly elongate, is [II I]. The calculated re-entrant angles on the two sides of the pseudotrigonal prism, the protruding angle on the third side, and the 'central misfit', expressed as the geometrical ngles, are I78 ~ 4I', I8I ~ 2o', and 2 ~ 39 ' respectively. Tetragonal crystals forming pseudotrigonal twins are rare and it is emphasized that the pseudotrigonal habit has become apparent only because: the faces developed on individual I and on individuals II and III are not the same; and the proportion between the lengths of the traces of the faces (io i) individual I and (oi I) individuals II and III in a plane perpendicular tothe pseudo-threefold axis and the traces in the same plane of all other faces constituting the pseudo-threefold prism are 2: i. TUGTUPITE (NasAlzBe2SisO24(CI, S)2), dis-covered in i957 by Professor H. Sorensen at Tugtup agtak6rfia on the north coast of the Tunugdliarfik Fjord, South Greenland, was de-scribed in the reports of the International Geo- Text Greenland Unknown Greenland Triplets ENVELOPE(-59.750,-59.750,-62.383,-62.383)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description logically to the crystal class 7~2m. The paper describes pseudotrigonal contact riplets recently found as freely developed individuals on two specimens donated to the Geological Museum, Copenhagen. The contact triplets, described as a symmetric twin, have the composition planes, which are also the twin planes, (io0 and (o I i); the pseudo-threefold axis, along which the crystals are pronouncedly elongate, is [II I]. The calculated re-entrant angles on the two sides of the pseudotrigonal prism, the protruding angle on the third side, and the 'central misfit', expressed as the geometrical ngles, are I78 ~ 4I', I8I ~ 2o', and 2 ~ 39 ' respectively. Tetragonal crystals forming pseudotrigonal twins are rare and it is emphasized that the pseudotrigonal habit has become apparent only because: the faces developed on individual I and on individuals II and III are not the same; and the proportion between the lengths of the traces of the faces (io i) individual I and (oi I) individuals II and III in a plane perpendicular tothe pseudo-threefold axis and the traces in the same plane of all other faces constituting the pseudo-threefold prism are 2: i. TUGTUPITE (NasAlzBe2SisO24(CI, S)2), dis-covered in i957 by Professor H. Sorensen at Tugtup agtak6rfia on the north coast of the Tunugdliarfik Fjord, South Greenland, was de-scribed in the reports of the International Geo-
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Ole V. Petersen
Space Group
Belongs Morpho
spellingShingle Ole V. Petersen
Space Group
Belongs Morpho
Geological Museum, Copenhagen
author_facet Ole V. Petersen
Space Group
Belongs Morpho
author_sort Ole V. Petersen
title Geological Museum, Copenhagen
title_short Geological Museum, Copenhagen
title_full Geological Museum, Copenhagen
title_fullStr Geological Museum, Copenhagen
title_full_unstemmed Geological Museum, Copenhagen
title_sort geological museum, copenhagen
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.601.3505
http://www.minersoc.org/pages/Archive-MM/Volume_42/42-322-251.pdf
long_lat ENVELOPE(-59.750,-59.750,-62.383,-62.383)
geographic Greenland
Triplets
geographic_facet Greenland
Triplets
genre Greenland
genre_facet Greenland
op_source http://www.minersoc.org/pages/Archive-MM/Volume_42/42-322-251.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.601.3505
http://www.minersoc.org/pages/Archive-MM/Volume_42/42-322-251.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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