sultry
发表于 2025-3-25 06:57:49
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AV-node
发表于 2025-3-25 08:54:35
https://doi.org/10.1007/978-3-031-18007-1Archean Greenstone; Crustal Evolution; Early Life; Pilbara Craton; Vaalbara
Incumbent
发表于 2025-3-25 12:42:08
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LAPSE
发表于 2025-3-25 19:06:08
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
发表于 2025-3-25 20:54:54
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Gentry
发表于 2025-3-26 02:08:52
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RECUR
发表于 2025-3-26 08:08:11
,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
发表于 2025-3-26 12:15:55
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
发表于 2025-3-26 15:26:07
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CT-angiography
发表于 2025-3-26 19:35:13
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