Titlebook: Archean Evolution of the Pilbara Craton and Fortescue Basin; Arthur H. Hickman Book 2023 Springer Nature Switzerland AG 2023 Archean Green

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Wellbeing in Politics and Policyinental microplates (East Pilbara, Karratha, and Kurrana Terranes) were separated by two expanding rift basins. Between the Karratha Terrane (KT) and the East Pilbara Terrane (EPT), the Regal Basin evolved from a spreading centre to form a belt of MORB-like basaltic crust. The early Mesoarchean Mosq

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https://doi.org/10.1007/978-3-030-21376-3 related to ongoing northwest–southeast compression of the Pilbara Craton. This compression is interpreted to have resulted from c. 3160 Ma collision and subsequent interaction with an exotic plate northwest of the craton. Following closure of the Regal Basin at c. 3070 Ma (Chap. .), geochronologica

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Wellbeing in Politics and PolicyMa Mosquito Creek Orogeny. The deformation of these events compressed and closed the Mallina and Mosquito Creek Basins and effectively completed cratonization. From 2900 Ma onwards, the Pilbara Craton remained a stable unit of continental crust until uplift, crustal extension, and rifting began the

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https://doi.org/10.1007/978-3-030-21376-3 c. 2775 and 2710 Ma, mafic–felsic volcanic and intrusive activity continued in stages that were separated by periods of uplift, folding, erosion, and sedimentation. The first basaltic formation deposited across the eroded surface of the craton was the Mount Roe Basalt, up to 2.44 km thick and fed f

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