Geology, mining history and mineral potential of LCC Alpine Study Area
Laing, A. C. M.

Geology, mining history and mineral potential of LCC Alpine Study Area

Laing, A. C. M.

Personal Author
Laing, A. C. M.

Publication Information
Melbourne: Geological Survey of Victoria, 1975.

Physical Description
1 v. : 1 document.

Geological Survey of Victoria Unpublished Report 1975/50

General Note
(Reference Abstract -- Abstract ) The northwest trending belt of metamorphic rocks about 35km wide through Omeo between Towanga and Ensay is the dominant geological feature of the Alpine study area. This metamorphic belt comsists of schist and gneiss believed to be Ordovician in age intruded by younger granites and other plutonic rocks. It is flanked to east and west successively by less metomorphosed Ordocician sediments, by Devonian volcanics and Devonian and Lower Carboniferous sediments, through the post Ordovician pre Permian geological history has been different on either flank.

LibraryMaterial TypeItem BarcodeShelf NumberCopyChild SiteChild CountShelf LocationItem Category 1Item AvailableStatus
607 Sneydes Rd WerribeeManuscript110463-2001DR UR 1975/501VGLS1Request itemDPI1Request item
607 Sneydes Rd WerribeeManuscript110463-3001DRMJ UR 1975/501VGLS1Microform collectionDPI1Microform collection
607 Sneydes Rd WerribeeMicroform110463-4001DRMJ UR 1975/501VGLS1MFSET4DPI1MFSET4