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001461368 001__ 1461368
001461368 003__ OCoLC
001461368 005__ 20230503003349.0
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001461368 019__ $$a1372548927$$a1372622443
001461368 020__ $$a9783031180071$$q(electronic bk.)
001461368 020__ $$a3031180070$$q(electronic bk.)
001461368 020__ $$z9783031180057
001461368 020__ $$z3031180054
001461368 0247_ $$a10.1007/978-3-031-18007-1$$2doi
001461368 035__ $$aSP(OCoLC)1372549513
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001461368 049__ $$aISEA
001461368 050_4 $$aQE653.3
001461368 08204 $$a551.7/12$$223/eng/20230314
001461368 1001_ $$aHickman, Arthur H.$$q(Arthur Hugh),$$d1947-$$eauthor.$$1https://isni.org/isni/0000000063622414
001461368 24510 $$aArchean evolution of the Pilbara Craton and Fortescue Basin /$$cArthur H. Hickman.
001461368 264_1 $$aCham :$$bSpringer,$$c[2023]
001461368 264_4 $$c©2023
001461368 300__ $$a1 online resource (xlv, 465 pages) :$$billustrations (chiefly color).
001461368 336__ $$atext$$btxt$$2rdacontent
001461368 337__ $$acomputer$$bc$$2rdamedia
001461368 338__ $$aonline resource$$bcr$$2rdacarrier
001461368 4901_ $$aModern approaches in solid earth sciences ;$$vvolume 24
001461368 504__ $$aIncludes bibliographical references.
001461368 5050_ $$aChapter 1. Overview Of The Pilbara Craton -- Chapter 2. Eoarchean And Early Paleoarchean Crust Of The Pilbara Craton -- Chapter 3. Warrawoona Large Igneous Province, 35303427 Ma -- Chapter 4. Strelley Pool Formation: Continental Sedimentation Between Paleoarchean Lips -- Chapter 5. Kelly Large Igneous Province, 33503315 Ma -- Chapter 6. Paleoarchean Continental Breakup Of The Pilbara Craton -- Chapter 7. Mesoarchean Rift And Marginal Basins Of The Pilbara Craton -- Chapter 8. Mesoarchean Subduction In The Pilbara Craton -- Chapter 9. Mesoarchean Basin Evolution Inland Of Magmatic Arcs -- Chapter 10. Orogenies, Cratonization And Post-Orogenic Granites -- Chapter 11. Mineralization In The Northern Pilbara -- Chapter 12. Fortescue Group: The Neoarchean Breakup Of The Pilbara Craton.
001461368 506__ $$aAccess limited to authorized users.
001461368 520__ $$aOne of todays major geoscientific controversies centres on the origin of the Archean granitegreenstone terranes. Is the geology of these scattered remnants of our planets early crust consistent with the theory that modern-style plate-tectonic processes operated from the early Archean, or does it indicate that tectonic and magmatic processes were different in the Archean? Earth has clearly evolved since its initial formation, so at what stage did its processes of crustal growth first resemble those of today? The logical place to seek answers to these intriguing and important questions is within the best-preserved early Archean crust. The Pilbara region of northwest Australia is internationally famous for its abundant and exceptionally well-preserved fossil evidence of early life. However, until recently the area has received much less recognition for the key evidence it provides on early Archean crustal evolution. This book presents and interprets this evidence through a new stage-by-stage account of the development of the Pilbaras geological record between 3.53 and 2.63 Ga. The Archean Pilbara crust represents one fragment of Earths oldest known supercontinent Vaalbara, which also included the Kaapvaal Craton of southern Africa. Recognition of Vaalbara expands the background database for both these areas, allowing us to more fully understand each of them. .
001461368 588__ $$aDescription based on print version record.
001461368 650_0 $$aGeology, Stratigraphic$$yArchaean.
001461368 650_0 $$aPhysical geology$$zAustralia$$zPilbara (W.A.)
001461368 650_0 $$aPhysical geology$$zAustralia$$zFortescue River Watershed (W.A.)
001461368 655_0 $$aElectronic books.
001461368 77608 $$iPrint version:$$aHickman, Arthur H. (Arthur Hugh), 1947-$$tArchean evolution of the Pilbara Craton and Fortescue Basin.$$dCham : Springer, 2022$$z9783031180057$$w(OCoLC)1348996137
001461368 830_0 $$aModern approaches in solid earth sciences ;$$vv. 24.
001461368 852__ $$bebk
001461368 85640 $$3Springer Nature$$uhttps://univsouthin.idm.oclc.org/login?url=https://link.springer.com/10.1007/978-3-031-18007-1$$zOnline Access$$91397441.1
001461368 909CO $$ooai:library.usi.edu:1461368$$pGLOBAL_SET
001461368 980__ $$aBIB
001461368 980__ $$aEBOOK
001461368 982__ $$aEbook
001461368 983__ $$aOnline
001461368 994__ $$a92$$bISE