Please use this identifier to cite or link to this item: https://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1767
Title: The geology of the Rockwell 1:25,000 sheet area, Broken Hill, New South Wales
Other Titles: The geology of the Rockwell
Authors: G. Bradley
Geological Survey of NSW
Keywords: Rockwell 1:25,000 sheet;Broken Hill
Issue Date: 1982
Publisher: Department of Mineral resources
Abstract: This report contains descriptions of the rock units mapped in the Rockwell 1:25,000 sheet area. The rock units include meta sediments, composite gneisses, migmatites, quartzo-feldspathjc gneisses, leucocratic quartzo-feldspathjc rocks, basic and ultrabasic rocks, mineralized rocks, and retrograde schists. Interpretations of metamorphism, stratigraphy, and structure are very briefly outlined. Mineralization is largely stratiform Broken Hill type Pb-Zn-Ag which is spatially associated with quartz-gahnite rock, garnet-quartz rock, and "banded iron formation". Minor Cu mineralization occurs with pyrrhotite in garnet-quartz rocks and/or quartz-magnetjte rocks.
Internal ID Number: 81160
GS 1982/342
URI: https://nswdpe.intersearch.com.au/nswdpejspui/handle/1/1767
Appears in Collections:Geological Survey of NSW [1874 -present]

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