Dynamothermal transition zone between Archaean greenstone and granitoid gneiss at Lake Dundas, Western Australia
- 1 January 1985
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 7 (2), 187-203
- https://doi.org/10.1016/0191-8141(85)90131-2
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Gliding and overthrust nappe tectonics in the Barberton Greenstone BeltJournal of Structural Geology, 1982
- Archaean greenstone belts: A structaral test of tectonic hypothesisTectonophysics, 1980
- Thermal and mechanical evolution of shear zonesJournal of Structural Geology, 1980
- Horizontal tectonic interaction of an Archean gneiss belt and greenstones, Pilbara block, Western AustraliaGeology, 1980
- Structure and tectonic style of the Western Australian ShieldTectonophysics, 1979
- Archaean tectonics in the Agnew supracrustal belt, Western AustraliaPrecambrian Research, 1978
- Ultramafic rocks of the Widgiemooltha-Norseman area, Western Australia: Petrological diversity, geochemistry and mineralisationPrecambrian Research, 1978
- Indirect evidence for tectonic reactivation of a pre-greenstone sialic basement in Western AustraliaEarth and Planetary Science Letters, 1977
- Alpine-type structures in the Rhodesian basement complex at SelukweJournal of the Geological Society, 1974
- The Jimberlana Norite, Western Australia – a smaller analogue of the Great Dyke of Rhodesia.Geological Magazine, 1970