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Marshall, Patrick (1929) The occurrence of a mineral hitherto unrecognized in the phonolites of Dunedin, New Zealand. Mineralogical Magazine and Journal of the Mineralogical Society, 22 (127) 174-178 doi:10.1180/minmag.1929.022.127.02

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Reference TypeJournal (article/letter/editorial)
TitleThe occurrence of a mineral hitherto unrecognized in the phonolites of Dunedin, New Zealand
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsMarshall, PatrickAuthor
Year1929 (December)Volume22
Issue127
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_22/22-127-174.pdf+
DOIdoi:10.1180/minmag.1929.022.127.02
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Mindat Ref. ID7084Long-form Identifiermindat:1:5:7084:7
GUID0
Full ReferenceMarshall, Patrick (1929) The occurrence of a mineral hitherto unrecognized in the phonolites of Dunedin, New Zealand. Mineralogical Magazine and Journal of the Mineralogical Society, 22 (127) 174-178 doi:10.1180/minmag.1929.022.127.02
Plain TextMarshall, Patrick (1929) The occurrence of a mineral hitherto unrecognized in the phonolites of Dunedin, New Zealand. Mineralogical Magazine and Journal of the Mineralogical Society, 22 (127) 174-178 doi:10.1180/minmag.1929.022.127.02
In(1929) Mineralogical Magazine Vol. 22 (127) Mineralogical Society
Abstract/NotesThe phonolites which are found in the volcanic region of Dunedin, New Zealand, are of a varied character. Some of them are of ordinary types, but others are nephelinitoid, and some of them have sodalite in abundance. Besides the phonolites, there are trachydolerites, some of which also contain sodalite as well as nepheline. There is also an abundance of tinguaites, in all of which nepheline is distinct and sometimes sodalite as well. All petrologists who have worked in this region are therefore perfectly familiar with the minerals sodalite and nepheline in many different associations and conditions.


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