The Kararan orogeny was an orogenic event in the Gawler Craton of South Australia during the Proterozoic between 1.57 and 1.55 billion years ago which reworked rocks metamorphosed during the Kimban orogeny.
[1][2]
^Payne, J.L. and co-authors (2007). "Temporal constraints on the timing of high-grade metamorphism in the northern Gawler Craton: implications for assembly of the Australian Proterozoic". Australian Journal of Earth Sciences. 55 (5): 623. doi:10.1080/08120090801982595.
^Myers, John S.; Shaw, Russell D.; Tyler, Ian M. (1996). "Tectonic evolution of Proterozoic Australia". Tectonics. 15 (6): 1431–1446. Bibcode:1996Tecto..15.1431M. doi:10.1029/96TC02356.
The Kararanorogeny was an orogenic event in the Gawler Craton of South Australia during the Proterozoic between 1.57 and 1.55 billion years ago which...
heavily sheared orthoclase porphyroclastic granites c. 1,650 Ma – KararanOrogeny (1.65 Gyr) uplifts great mountains on the Gawler Craton in Southern...
Orogeny, 1,680–1,620 Ma, on the Gascoyne Complex in Western Australia. KararanOrogeny (1,650 Ma), Gawler Craton, South Australia. Oxygen levels drop again...
central Craton, the Yarlbrinda Shear Zone was likely formed by the KararanOrogeny and it is host to several major gold prospects including those in the...
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