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  • 1
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Plate tectonics. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (362 pages)
    Edition: 1st ed.
    ISBN: 9781444324877
    DDC: 551.21
    Language: English
    Note: Plates vs. Plumes: A Geological Controversy -- Contents -- Preface -- 1: From plate tectonics to plumes, and back again -- 1.1 Volcanoes, and exceptional volcanoes -- 1.2 Early beginnings: Continental drift and its rejection -- 1.3 Emergence of the Plume hypothesis -- 1.4 Predictions of the Plume hypothesis -- 1.5 Lists of plumes -- 1.6 Testing plume predictions -- 1.7 A quick tour of Hawaii and Iceland -- 1.8 Moving on: Holism and alternatives -- 1.9 The Plate hypothesis -- 1.10 Predictions of the Plate hypothesis -- 1.11 Testing the Plate hypothesis -- 1.12 Revisiting Hawaii and Iceland -- 1.13 Questions and problems -- 1.14 Exercises for the student -- 2: Vertical motions -- 2.1 Introduction -- 2.2 Predictions of the Plume hypothesis -- 2.3 Predictions of the Plate hypothesis -- 2.4 Comparison of the predictions of the Plume and Plate hypotheses -- 2.5 Observations -- 2.5.1 Classifying melting anomalies -- 2.5.2 Volcanic chains with initial flood basalts -- 2.5.3 Volcanic chains without initial flood basalts -- 2.5.4 Active flood basalt provinces lacking volcanic chains -- 2.5.5 Extinct flood basalt provinces lacking volcanic chains -- 2.5.6 Vertical motions without flood basalt magmatism -- 2.6 Plume variants -- 2.7 Discussion -- 2.8 Exercises for the student -- 3: Volcanism -- 3.1 Introduction -- 3.1.1 Flood basalts and oceanic plateaus -- 3.1.2 Normal or anomalous? -- 3.2 Predictions of the Plume hypothesis -- 3.3 Predictions of the Plate hypothesis -- 3.4 Comparison of the predictions of the Plate and Plume hypotheses -- 3.5 Observations -- 3.5.1 Classifying melting anomalies -- 3.5.2 Large-volume, sustained volcanism -- 3.5.3 Large-volume, brief volcanism -- 3.5.4 Small-volume, sustained volcanism -- 3.5.5 Small-volume, brief volcanism -- 3.6 Plume variants -- 3.7 Discussion -- 3.8 Exercises for the student. , 4: Time progressions and relative fixity of melting anomalies -- 4.1 Introduction -- 4.2 Methods -- 4.2.1 Radiometric dating -- 4.2.2 Earth's palaeomagnetic and spin axes -- 4.2.3 True polar wander -- 4.3 Predictions of the Plume hypothesis -- 4.4 Predictions of the Plate hypothesis -- 4.5 Observations -- 4.5.1 Melting anomalies without tracks -- 4.5.2 Short-lived melting anomalies -- 4.5.3 Melting anomalies with long chains that are not time-progressive -- 4.5.4 Melting anomalies with long, time-progressive tracks -- 4.6 Hotspot reference frames -- 4.7 Plume variants -- 4.7.1 "Mantle wind" -- 4.7.2 Other variants -- 4.8 Discussion -- 4.9 Exercises for the student -- 5: Seismology -- 5.1 Introduction -- 5.1.2 Seismology is not a thermometer -- 5.2 Seismological techniques -- 5.2.1 Explosion seismology -- 5.2.2 Tomography -- 5.2.3 Teleseismic tomography -- 5.2.4 Whole-mantle tomography -- 5.2.5 Presenting tomography results -- 5.2.6 Receiver functions -- 5.2.7 Shear-wave splitting -- 5.3 Predictions of the Plume hypothesis -- 5.4 Predictions of the Plate hypothesis -- 5.5 Observations -- 5.5.1 Well-studied melting anomalies on extensive land masses -- 5.5.2 Less well-studied melting anomalies in remote regions -- 5.5.3 Structure beneath extinct melting anomalies, and elsewhere -- 5.6 Global observations -- 5.6.1 Whole-mantle tomography -- 5.6.2 Global variations in the transition zone -- 5.6.3 The core-mantle boundary -- 5.7 Plume variants -- 5.8 Discussion -- 5.9 Exercises for the student -- 6: Temperature and heat -- 6.1 Introduction -- 6.1.1 Surface heat loss -- 6.1.2 Subsurface temperature profiles -- 6.1.3 Where is the melt? -- 6.1.4 Temperature and heat -- 6.2 Methods -- 6.2.1 Seismology -- 6.2.2 Petrological and geochemical methods -- 6.2.3 Ocean floor bathymetry -- 6.2.4 Heat flow -- 6.2.5 Heat loss from intrusions and eruptives. , 6.3 Predictions of the Plume hypothesis -- 6.4 Predictions of the Plate hypothesis -- 6.5 Observations -- 6.5.1 Mid-ocean ridges -- 6.5.2 The North Atlantic Igneous Province -- 6.5.3 Hawaii -- 6.5.4 Oceanic plateaus -- 6.5.5 Swells -- 6.6 Variants of the Plume hypothesis -- 6.7 Discussion -- 6.8 Exercises for the student -- 7: Petrology and geochemistry -- 7.1 Introduction -- 7.2 Some basics -- 7.2.1 Tholeiite and alkali basalts -- 7.2.2 Mantle composition and heterogeneity -- 7.2.3 From melt to source rocks -- 7.2.4 Trace elements and rare-earth elements -- 7.2.5 Radiogenic isotope ratios -- 7.2.6 The mantle zoo -- 7.2.7 MORB, OIB, tholeiites and alkali basalt -- 7.3 Predictions of the Plume hypothesis -- 7.4 Predictions of the Plate hypothesis -- 7.5 Proposed deep-mantle- and core-mantle-boundary tracers -- 7.5.1 Helium (He) isotope ratios -- 7.5.2 Neon (Ne) isotope ratios -- 7.5.3 The Rhenium-Osmium (Re-Os), Platinum-Osmium (Pt-Os) and Hafnium-Tungsten (Hf-W) isotope systems -- 7.6 A few highlights from melting anomalies -- 7.6.1 Iceland and Greenland -- 7.6.2 The Emperor and Hawaiian chains -- 7.6.3 Flood basalts -- 7.6.4 Back-arc regions -- 7.7 Plume variants -- 7.8 Discussion -- 7.9 Exercises for the student -- 8: Synthesis -- 8.1 Introduction -- 8.1.1 In the beginning -- 8.1.2 The rise and fall of plumes -- 8.1.3 The ins and outs: Volume -- 8.1.4 The when and where -- 8.1.5 Redium and blueium -- 8.1.6 Are "hot spots" hot? -- 8.1.7 Chemical messengers -- 8.2 Mantle convection -- 8.3 An unfalsifiable hypothesis -- 8.3.1 Building on sand -- 8.4 Diversity: as moking gun -- 8.5 The need for joined-up science -- 8.6 The future -- 8.7 Exercises for the student -- References -- Index -- Colour plate section.
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  • 2
    Publication Date: 2023-02-08
    Description: The breakup of Laurasia to form the Northeast Atlantic Realm disintegrated an inhomogeneous collage of cratons sutured by cross-cutting orogens. Volcanic rifted margins formed that are underlain by magma-inflated, extended continental crust. North of the Greenland-Iceland-Faroe Ridge a new rift–the Aegir Ridge–propagated south along the Caledonian suture. South of the Greenland-Iceland-Faroe Ridge the proto-Reykjanes Ridge propagated north through the North Atlantic Craton along an axis displaced ~150 km to the west of the rift to the north. Both propagators stalled where the confluence of the Nagssugtoqidian and Caledonian orogens formed an ~300-km-wide transverse barrier. Thereafter, the ~150 × 300-km block of continental crust between the rift tips–the Iceland Microcontinent–extended in a distributed, unstable manner along multiple axes of extension. These axes repeatedly migrated or jumped laterally with shearing occurring between them in diffuse transfer zones. This style of deformation continues to the present day in Iceland. It is the surface expression of underlying magma-assisted stretching of ductile continental crust that has flowed from the Iceland Microplate and flanking continental areas to form the lower crust of the Greenland-Iceland-Faroe Ridge. Icelandic-type crust which underlies the Greenland-Iceland-Faroe Ridge is thus not anomalously thick oceanic crust as is often assumed. Upper Icelandic-type crust comprises magma flows and dykes. Lower Icelandic-type crust comprises magma-inflated continental mid- and lower crust. Contemporary magma production in Iceland, equivalent to oceanic layers 2–3, corresponds to Icelandic-type upper crust plus intrusions in the lower crust, and has a total thickness of only 10–15 km. This is much less than the total maximum thickness of 42 km for Icelandic-type crust measured seismically in Iceland. The feasibility of the structure we propose is confirmed by numerical modeling that shows extension of the continental crust can continue for many tens of millions of years by lower-crustal ductile flow. A composition of Icelandic-type lower crust that is largely continental can account for multiple seismic observations along with gravity, bathymetric, topographic, petrological and geochemical data that are inconsistent with a gabbroic composition for Icelandic-type lower crust. It also offers a solution to difficulties in numerical models for melt-production by downward-revising the amount of melt needed. Unstable tectonics on the Greenland-Iceland-Faroe Ridge can account for long-term tectonic disequilibrium on the adjacent rifted margins, the southerly migrating rift propagators that build diachronous chevron ridges of thick crust about the Reykjanes Ridge, and the tectonic decoupling of the oceans to the north and south. A model of complex, discontinuous continental breakup influenced by crustal inhomogeneity that distributes continental material in growing oceans fits other regions including the Davis Strait, the South Atlantic and the West Indian Ocean.
    Type: Article , PeerReviewed
    Format: text
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  • 3
    Publication Date: 2023-01-02
    Description: We propose a new, sunken continent beneath the North Atlantic Ocean that we name Icelandia. It may comprise blocks of full-thickness continental lithosphere or extended, magma-inflated continental layers that form hybrid continental-oceanic lithosphere. It underlies the Greenland-Iceland-Faroe Ridge and the Jan Mayen microplate complex, covering an area of ~600,000 km2. It is contiguous with the Faroe Plateau and known parts of the submarine continental rifted margin offshore Britain. If these are included in a “Greater Icelandia,” the entire area is ~1,000,000 km2 in size. The existence of Icelandia needs to be tested. Candidate approaches include mag- netotelluric surveying in Iceland; ultralong, full-crust-penetrating reflection profiling along the length of the Greenland-Iceland-Faroe Ridge; dating zircons collected in Ice- land; deep drilling; and reappraisal of the geology of Iceland. Some of these methods could be applied to other candidate sunken continents that are common in the oceans.
    Type: Book chapter , NonPeerReviewed
    Format: text
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