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標題: Titlebook: Archean Evolution of the Pilbara Craton and Fortescue Basin; Arthur H. Hickman Book 2023 Springer Nature Switzerland AG 2023 Archean Green [打印本頁]

作者: Opiate    時間: 2025-3-21 20:03
書目名稱Archean Evolution of the Pilbara Craton and Fortescue Basin影響因子(影響力)




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書目名稱Archean Evolution of the Pilbara Craton and Fortescue Basin讀者反饋




書目名稱Archean Evolution of the Pilbara Craton and Fortescue Basin讀者反饋學科排名





作者: ARY    時間: 2025-3-21 22:34

作者: mitten    時間: 2025-3-22 01:08

作者: Lament    時間: 2025-3-22 04:36

作者: Infinitesimal    時間: 2025-3-22 12:45

作者: 榮幸    時間: 2025-3-22 13:19
Book 2023emnants of our planet’s early crust consistent with the theory that modern-style plate-tectonic processes operated from the early Archean, or does it indicate that tectonic and magmatic processes were different in the Archean? Earth has clearly evolved since its initial formation, so at what stage d
作者: 掃興    時間: 2025-3-22 20:35

作者: 防止    時間: 2025-3-22 23:31
Evidence in the Age of the New Sciencesears before deposition of the greenstone succession (3530–3235?Ma Pilbara Supergroup). Dates on pre-3530?Ma xenocrystic zircons in felsic igneous rocks and detrital zircons in Paleoarchean and Mesoarchean metasedimentary rocks suggest that this early crust evolved from about 3800?Ma. Zircon ages sug
作者: 新星    時間: 2025-3-23 03:15
Evidence in the Age of the New Sciencesleoarchean greenstone succession of the East Pilbara Terrane and is preserved in 20 greenstone belts. The group was erupted across the entire area of the 3800–3530?Ma Pilbara crust (Chap. .), and its thickness varies between 10 and 15?km. Variations are partly due to local erosional unconformities t
作者: Suppository    時間: 2025-3-23 08:27

作者: 負擔    時間: 2025-3-23 09:49

作者: ADORE    時間: 2025-3-23 15:25

作者: 糾纏    時間: 2025-3-23 19:38
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
作者: 人工制品    時間: 2025-3-23 23:54

作者: 不舒服    時間: 2025-3-24 05:32
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
作者: 褻瀆    時間: 2025-3-24 09:05
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
作者: Decibel    時間: 2025-3-24 11:01

作者: 紅腫    時間: 2025-3-24 18:07
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
作者: 合同    時間: 2025-3-24 22:38

作者: occult    時間: 2025-3-25 01:19

作者: sultry    時間: 2025-3-25 06:57

作者: AV-node    時間: 2025-3-25 08:54
https://doi.org/10.1007/978-3-031-18007-1Archean Greenstone; Crustal Evolution; Early Life; Pilbara Craton; Vaalbara
作者: Incumbent    時間: 2025-3-25 12:42

作者: LAPSE    時間: 2025-3-25 19:06
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
作者: 假    時間: 2025-3-25 20:54

作者: Gentry    時間: 2025-3-26 02:08

作者: RECUR    時間: 2025-3-26 08:08
,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
作者: Bernstein-test    時間: 2025-3-26 12:15
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
作者: regale    時間: 2025-3-26 15:26

作者: CT-angiography    時間: 2025-3-26 19:35

作者: 消瘦    時間: 2025-3-26 23:00

作者: 撤退    時間: 2025-3-27 02:32

作者: 重疊    時間: 2025-3-27 06:52

作者: 血統(tǒng)    時間: 2025-3-27 09:58
Evidence in the Age of the New Sciences 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
作者: 荒唐    時間: 2025-3-27 13:58
Evidence in the Age of the New Sciencess reveal that many of the TTG intrusions were subvolcanic to the felsic volcanic formations..The East Pilbara Terrane is now exposed across 40,000?km. of the northeast section of the Pilbara Craton, with concealed parts estimated to occupy an additional 60,000?km.. With an interpreted total volume o
作者: 要塞    時間: 2025-3-27 17:47

作者: evasive    時間: 2025-3-28 00:13
Marike van der Schaaf,Juultje Sommersis 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
作者: 新鮮    時間: 2025-3-28 03:51
Marike van der Schaaf,Juultje Sommers 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
作者: ESPY    時間: 2025-3-28 06:54

作者: overshadow    時間: 2025-3-28 10:41

作者: 種類    時間: 2025-3-28 17:14

作者: 可商量    時間: 2025-3-28 21:14
Wellbeing in Politics and Policyvironments and were formed as thin, low-grade, and laterally discontinuous units..The most significant mineralization in the Neoarchean Fortescue Group is conglomerate-hosted gold, although sub-economic uranium mineralization is also present in some conglomerates.
作者: Pander    時間: 2025-3-29 01:09
https://doi.org/10.1007/978-3-030-21376-3both areas. Almost all volcanic activity ended at c. 2710?Ma following eruption of the Maddina Formation of the North Pilbara (correlated with the Bunjinah Formation in the south). Between c. 2710 and 2630?Ma, mainly clastic sedimentary rocks of the Jeerinah Formation, the upper formation of the For
作者: MIRTH    時間: 2025-3-29 03:37

作者: 口味    時間: 2025-3-29 10:50
1876-1682 ew stage-by-stage account of the development of the Pilbara’s geological record between 3.53 and 2.63 Ga.. The Archean Pilbara crust represents one fragment of Earth’s oldest known supercontinent Vaalbara, whic978-3-031-18007-1Series ISSN 1876-1682 Series E-ISSN 1876-1690
作者: 踉蹌    時間: 2025-3-29 12:18





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