The Petrology and Mineralization of The Coolac Serpentine Belt East of Brungle, New South Wales
- Organization:
- The Australasian Institute of Mining and Metallurgy
- Pages:
- 20
- File Size:
- 5145 KB
- Publication Date:
- Jan 1, 1969
Abstract
A belt of serpentinized ultrabasic rocks intrudes a moderately folded geosynclinal sequence of fine to coarse sediments, acid, intermediate, and basic volcanics as well as a batholithic mass of granitic rocks. The ultrabasic body contains small included masses of melanocratic and leucocratic rocks, together with chromium, copper, zinc, and nickel mineralization.
Citation
APA: (1969) The Petrology and Mineralization of The Coolac Serpentine Belt East of Brungle, New South Wales
MLA: The Petrology and Mineralization of The Coolac Serpentine Belt East of Brungle, New South Wales. The Australasian Institute of Mining and Metallurgy, 1969.