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Volcano-sedimentary successions of the Bryah and Padbury Groups were deposited and deformed along the northern margin of Archaean Yilgarn Craton, Western Australia, during the ca 2.0-1.8 Ga Capricorn Orogeny. This orogeny is interpreted to record convergence and collision of the Yilgarn Craton with the Pilbara Craton to the north. The Bryah Group with its extensive mafic and ultramafic volcanic rocks...
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