Please use this identifier to cite or link to this item: https://nswdpe.intersearch.com.au/nswdpejspui/handle/1/2552
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dc.contributor.authorW. J. Stroud-
dc.date.accessioned2023-06-21T13:10:08Z-
dc.date.available2023-06-21T13:10:08Z-
dc.date.issued1980-
dc.identifier.urihttps://nswdpe.intersearch.com.au/nswdpejspui/handle/1/2552-
dc.descriptionAbstract The Glen Idol 1:25,000 sheet area consists of polymetamorphosed and highly deformed sediments and volcanics. The rock units include metasediments, composite gneisses, quartzo-feldspathic gneisses and rocks, amphibolites and iron rich rocks. These comprise parts of the Euriowie and Broken Hill Blocks of the Willyama Complex. They are unconformably overlain by Adelaidean sediments. A stratigraphic sequence can be correlated with that of Stevens et al. (I98O). Although no "Mine Sequence" suite is present, an elongate pyrite-rich horizon is present in the Euriowie Block. This horizon and the rocks that contain it may warrant detailed prospecting.-
dc.source/mnt/conversions/nswdpe/20220815_1_DPIE//Scanned Files/Box 55/Geology of the Glen Idol 1 25000 Sheet Area Broken Hill NSW.pdfen
dc.subjectMap Reference:  Broken Hill SH 54-15 7234-II-Nen
dc.subjectGS  1980/141en
dc.titleGeology of the Glen Idol 1 25000 Sheet Area Broken Hill NSWen
dc.typepdfen
dc.contributor.corpauthorDepartment of Mineral Resources NSW-
dc.contributor.corpauthorGeological Survey of NSW-
Appears in Collections:Geological Survey of NSW [1874 -present]

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