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Archean evolution of the Pilbara Cra...

Hickman, Arthur H.

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Archean evolution of the Pilbara Craton and Fortescue Basin

Record Type:	Electronic resources : Monograph/item
Title/Author:	Archean evolution of the Pilbara Craton and Fortescue Basin/ by Arthur H. Hickman.
Author:	Hickman, Arthur H.
Published:	Cham :Springer International Publishing : : 2023.,
Description:	xlv, 465 p. :ill. (chiefly col.), digital ;24 cm.
[NT 15003449]:	Chapter 1. Overview Of The Pilbara Craton -- Chapter 2. Eoarchean And Early Paleoarchean Crust Of The Pilbara Craton -- Chapter 3. Warrawoona Large Igneous Province, 3530-3427 Ma -- Chapter 4. Strelley Pool Formation: Continental Sedimentation Between Paleoarchean Lips -- Chapter 5. Kelly Large Igneous Province, 3350-3315 Ma -- Chapter 6. Paleoarchean Continental Breakup Of The Pilbara Craton -- Chapter 7. Mesoarchean Rift And Marginal Basins Of The Pilbara Craton -- Chapter 8. Mesoarchean Subduction In The Pilbara Craton -- Chapter 9. Mesoarchean Basin Evolution Inland Of Magmatic Arcs -- Chapter 10. Orogenies, Cratonization And Post-Orogenic Granites -- Chapter 11. Mineralization In The Northern Pilbara -- Chapter 12. Fortescue Group: The Neoarchean Breakup Of The Pilbara Craton.
Contained By:	Springer Nature eBook
Subject:	Geology, Stratigraphic - Archaean. -
Online resource:	https://doi.org/10.1007/978-3-031-18007-1
ISBN:	9783031180071

Archean evolution of the Pilbara Craton and Fortescue Basin
Hickman, Arthur H.

Archean evolution of the Pilbara Craton and Fortescue Basin[electronic resource] /by Arthur H. Hickman. - Cham :Springer International Publishing :2023. - xlv, 465 p. :ill. (chiefly col.), digital ;24 cm. - Modern approaches in solid earth sciences,v. 241876-1690 ;. - Modern approaches in solid earth sciences ;v. 24..

Chapter 1. Overview Of The Pilbara Craton -- Chapter 2. Eoarchean And Early Paleoarchean Crust Of The Pilbara Craton -- Chapter 3. Warrawoona Large Igneous Province, 3530-3427 Ma -- Chapter 4. Strelley Pool Formation: Continental Sedimentation Between Paleoarchean Lips -- Chapter 5. Kelly Large Igneous Province, 3350-3315 Ma -- Chapter 6. Paleoarchean Continental Breakup Of The Pilbara Craton -- Chapter 7. Mesoarchean Rift And Marginal Basins Of The Pilbara Craton -- Chapter 8. Mesoarchean Subduction In The Pilbara Craton -- Chapter 9. Mesoarchean Basin Evolution Inland Of Magmatic Arcs -- Chapter 10. Orogenies, Cratonization And Post-Orogenic Granites -- Chapter 11. Mineralization In The Northern Pilbara -- Chapter 12. Fortescue Group: The Neoarchean Breakup Of The Pilbara Craton.

One of today's major geoscientific controversies centres on the origin of the Archean granite-greenstone terranes. Is the geology of these scattered remnants 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 did its processes of crustal growth first resemble those of today? The logical place to seek answers to these intriguing and important questions is within the best-preserved early Archean crust. The Pilbara region of northwest Australia is internationally famous for its abundant and exceptionally well-preserved fossil evidence of early life. However, until recently the area has received much less recognition for the key evidence it provides on early Archean crustal evolution. This book presents and interprets this evidence through a new 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, which also included the Kaapvaal Craton of southern Africa. Recognition of Vaalbara expands the background database for both these areas, allowing us to more fully understand each of them.

ISBN: 9783031180071

Standard No.: 10.1007/978-3-031-18007-1doiSubjects--Topical Terms:

602876
Geology, Stratigraphic
--Archaean.

LC Class. No.: QE653.3

Dewey Class. No.: 551.712

Archean evolution of the Pilbara Craton and Fortescue Basin
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245 1 0 $a Archean evolution of the Pilbara Craton and Fortescue Basin $h [electronic resource] / $c by Arthur H. Hickman.
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505 0 $a Chapter 1. Overview Of The Pilbara Craton -- Chapter 2. Eoarchean And Early Paleoarchean Crust Of The Pilbara Craton -- Chapter 3. Warrawoona Large Igneous Province, 3530-3427 Ma -- Chapter 4. Strelley Pool Formation: Continental Sedimentation Between Paleoarchean Lips -- Chapter 5. Kelly Large Igneous Province, 3350-3315 Ma -- Chapter 6. Paleoarchean Continental Breakup Of The Pilbara Craton -- Chapter 7. Mesoarchean Rift And Marginal Basins Of The Pilbara Craton -- Chapter 8. Mesoarchean Subduction In The Pilbara Craton -- Chapter 9. Mesoarchean Basin Evolution Inland Of Magmatic Arcs -- Chapter 10. Orogenies, Cratonization And Post-Orogenic Granites -- Chapter 11. Mineralization In The Northern Pilbara -- Chapter 12. Fortescue Group: The Neoarchean Breakup Of The Pilbara Craton.
520 $a One of today's major geoscientific controversies centres on the origin of the Archean granite-greenstone terranes. Is the geology of these scattered remnants 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 did its processes of crustal growth first resemble those of today? The logical place to seek answers to these intriguing and important questions is within the best-preserved early Archean crust. The Pilbara region of northwest Australia is internationally famous for its abundant and exceptionally well-preserved fossil evidence of early life. However, until recently the area has received much less recognition for the key evidence it provides on early Archean crustal evolution. This book presents and interprets this evidence through a new 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, which also included the Kaapvaal Craton of southern Africa. Recognition of Vaalbara expands the background database for both these areas, allowing us to more fully understand each of them.
650 0 $a Geology, Stratigraphic $y Archaean. $3 602876
650 0 $a Physical geology $z Australia $z Pilbara (W.A.) $3 3631014
650 0 $a Physical geology $z Australia $z Fortescue River Watershed (W.A.) $3 3631015
650 1 4 $a Geodynamics. $3 539085
650 2 4 $a Geology. $3 516570
650 2 4 $a Petrology. $3 535210
650 2 4 $a Paleontology. $3 518862
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