Please use this identifier to cite or link to this item: https://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1351
Title: Reinterpretation of “pegmatite” in the centennial-Allendale portion of the Broken Hill Block
Other Titles: Quarterly Notes 30 Geological Survey of New South Wales 1st January 1978
Quarterly Notes 30
Authors: Department of Mines
Geological Survey of NSW
Keywords: quartz and feldspar;leucocratic quartzo-feldspathic rock;Broken Hill Block;pegmatite;coarse granitic-textured rock
Issue Date: 1978
Series/Report no.: Quarterly Notes
Abstract: Bodies 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.
URI: https://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1351
ISSN: 0155-3410
Appears in Collections:Geological Survey of NSW [1874 -present]

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