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.accessioned2023-06-21T10:45:20Z-
dc.date.available2023-06-21T10:45:20Z-
dc.date.issued1978en
dc.identifier.issn0155-3410-
dc.identifier.urihttps://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1351-
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.-
dc.relation.ispartofseriesQuarterly Notes-
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 Block-
dc.subjectpegmatite-
dc.subjectcoarse granitic-textured rock-
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 1978-
dc.title.alternativeQuarterly Notes 30-
dc.typepdfen
dc.contributor.corpauthorDepartment of Mines-
dc.contributor.corpauthorGeological Survey of NSW-
Appears in Collections:Geological Survey of NSW [1874 -present]

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