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

sultry

AV-node

https://doi.org/10.1007/978-3-031-18007-1Archean Greenstone; Crustal Evolution; Early Life; Pilbara Craton; Vaalbara

Incumbent

LAPSE

Eoarchean and Early Paleoarchean Crust of the Pilbara Craton, evidence for an abrupt change in magma sources between 3550 and 3530?Ma, marking a major event in the early crustal evolution of the Pilbara Craton. The precise nature of this event is unclear, although one likely explanation is that uplift, crustal extension, and rifting of the 3800–3530?Ma crust

假

Gentry

RECUR

,Kelly Large Igneous Province, 3350–3315?Ma,is restricted to the eastern half of the East Pilbara Terrane and was derived from partial melting of older felsic crust. Eruption of the Wyman Formation was accompanied by numerous granodiorite and monzogranite intrusions of the Emu Pool Supersuite. Geochronology indicates that in some of the East

Bernstein-test

Paleoarchean Continental Breakup of the Pilbara Craton, of continental crust and the evolution of intervening basaltic basins. It marked the beginning of plate tectonic processes in which Paleoarchean vertical deformation and crustal recycling were replaced by Mesoarchean horizontal deformation and melts derived from plate separation, collision, and sub

regale

CT-angiography