Please use this identifier to cite or link to this item: https://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1351
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dc.date.accessioned2023-06-21T10:45:20Zen
dc.date.available2023-06-21T10:45:20Zen
dc.date.issued1978en
dc.identifier.issn0155-3410en
dc.identifier.urihttps://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1351en
dc.description.abstractBodies of leucocratic quartzo-feldspathic rock with intermixed pegmatite occur in the Centennial - Allendale area. The bodies consist of three rock types: a fine to coarse-grained, foliated rock exhibiting schistosity, gneissosity, and/or layering; a coarse-grained rock with granitic texture and few or no planar elements; and coarse to very coarse-grained pegmatite.en
dc.relation.ispartofseriesQuarterly Notesen
dc.source/mnt/conversions/nswdpe/20220815_1_DPIE//Scanned Files/Box 32/Quarterly Notes 30 Geological Survey of New South Wales 1st January 1978.pdfen
dc.subjectquartz and feldsparen
dc.subjectleucocratic quartzo-feldspathic rocken
dc.subjectBroken Hill Blocken
dc.subjectpegmatiteen
dc.subjectcoarse granitic-textured rocken
dc.titleReinterpretation of “pegmatite” in the centennial-Allendale portion of the Broken Hill Blocken
dc.title.alternativeQuarterly Notes 30 Geological Survey of New South Wales 1st January 1978en
dc.title.alternativeQuarterly Notes 30en
dc.typepdfen
dc.contributor.corpauthorDepartment of Minesen
dc.contributor.corpauthorGeological Survey of NSWen
Appears in Collections:Geological Survey of NSW [1874 -present]

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