Tilba Tilba metamorphic and dyke complex; a new discovery

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doi: 10.1046/j.1440-0952.2001.00857.x
Authors:Rickard, M. J.
Author Affiliations:Primary:
University of Newcastle, Department of Geology, Newcastle, N.S.W., Australia
Volume Title:Australian Journal of Earth Sciences
Source:Australian Journal of Earth Sciences, 48(2), p.245-250. Publisher: Geological Society of Australia, Sydney, NSW, Australia. ISSN: 0812-0099
Publication Date:2001
Note:In English. 18 refs.; illus., incl. geol. sketch map
Summary:A small metamorphic and dyke complex of Ordovician age is exposed near Tilba Tilba on the S coast of New South Wales just E of the Cretaceous Mt Dromedary igneous complex. Mainly tonalites and granodiorites, the dykes intrude metaturbidites and spotted pelitic schists which have been tightly folded and crenulated in two episodes. The occurrence is the youngest and easternmost of high-grade metamorphic rocks in the Lachlan Fold Belt. [W.D.B.]
Subsections:Metamorphism: regional, dynamic
Subjects:Cretaceous; Devonian; Dikes; Granites; Igneous rocks; Intrusions; Mesozoic; Metamorphism; Mineral composition; P-T conditions; Paleozoic; Petrography; Phase equilibria; Plutonic rocks; Australasia; Australia; Lachlan fold belt; New South Wales Australia; Mount Dromedary; Tilba Tilba Complex
Coordinates:S370000 S360000 E1503000 E1493000
Abstract Numbers:01M/4706
Record ID:2003008780
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom
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