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Ghosh, P. K. (1927) Petrology of the Bodmin Moor granite (eastern part), Cornwall. Mineralogical Magazine and Journal of the Mineralogical Society, 21 (118) 285-309 doi:10.1180/minmag.1927.021.118.02

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Reference TypeJournal (article/letter/editorial)
TitlePetrology of the Bodmin Moor granite (eastern part), Cornwall
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsGhosh, P. K.Author
Year1927 (September)Volume21
Issue118
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_21/21-118-285.pdf+
DOIdoi:10.1180/minmag.1927.021.118.02
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Mindat Ref. ID7043Long-form Identifiermindat:1:5:7043:4
GUID0
Full ReferenceGhosh, P. K. (1927) Petrology of the Bodmin Moor granite (eastern part), Cornwall. Mineralogical Magazine and Journal of the Mineralogical Society, 21 (118) 285-309 doi:10.1180/minmag.1927.021.118.02
Plain TextGhosh, P. K. (1927) Petrology of the Bodmin Moor granite (eastern part), Cornwall. Mineralogical Magazine and Journal of the Mineralogical Society, 21 (118) 285-309 doi:10.1180/minmag.1927.021.118.02
In(1926) Mineralogical Magazine Vol. 21 (118) Mineralogical Society
Abstract/NotesThis paper presents the results of an investigation of the granite composing the eastern part of Bodmin Moor, Cornwall, as mapped on Sheet no. 337 of the Geological Survey. The work was undertaken on the suggestion of Dr. J.W. Evans, and comprised the field- and laboratory-work necessary for a detailed study of the petrology and tectonics of the area.The boundary of the granite, as mapped by the Geological Survey, has been retained, and also the distribution of the two main granite types ('coarse' and 'fine') shown on the Survey map. The coarse granite, however, has been sub-divided into two varieties, and it has been found practicable to map the distribution of each (fig. 1).The killas inclusions in this granite have not hitherto been studied, and these have received due attention. Similarly, the minor intrusions described include some that have not been previously recorded.


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