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Chapter 26 Palaeomagnetism and Precambrian Tectonic Evolution of Gondwana
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title
Chapter 26 Palaeomagnetism and Precambrian Tectonic Evolution of Gondwana
(English)
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main subject
Gondwana
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author name string
M.O. McWilliams
series ordinal
1
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publication date
1981
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published in
Neoproterozoic-Cambrian Tectonics, Global Change And Evolution: A Focus On South Western Gondwana
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page(s)
649-687
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cites work
Microplate tectonics, oblique collisions, and evolution of the Hercynian orogenic systems
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Discordant paleomagnetic pole positions as evidence of regional shear in the western Cordillera of North America
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Lithosphere Plate-Continental Margin Tectonics and the Evolution of the Appalachian Orogen
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Plate Tectonics and the Hercynian Orogeny
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Plume-Generated Triple Junctions: Key Indicators in Applying Plate Tectonics to Old Rocks
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Were Archean continental geothermal gradients much steeper than those of today?
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Evolution of the Appalachian/Caledonian Orogen
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Ophiolite obduction
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Mountain belts and the new global tectonics
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Origin and emplacement of the ophiolite suite: Appalachian ophiolites in Newfoundland
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Tibetan, Variscan, and Precambrian Basement Reactivation: Products of Continental Collision
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Pre-Mesozoic plate tectonics: How far back in Earth history can the Wilson Cycle be extended?
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Continental Collisions in the Appalachian-Caledonian Orogenic Belt: Variations Related to Complete and Incomplete Suturing
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Relations of andesites, granites, and derivative sandstones to arc-Trench tectonics
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Rubidium-Strontium Isochron Study of the Grenville Front near Lake Timagami, Ontario
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Paleopoles and paleolatitudes of North America and speculations about displaced terrains
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Polar Movement Relative to Australia
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Hairpins and Superintervals
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Sea-floor spreading and continental drift
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Precambrian geodynamics — a palaeomagnetic view
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The North Pacific: an Example of Tectonics on a Sphere
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Late Precambrian Paleomagnetism of Australia: The Adelaide Geosyncline
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Rises, trenches, great faults, and crustal blocks
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Palaeomagnetic Evidence for a Proterozoic Super-Continent [and Discussion]
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Collision of irregular continental margins: Implications for foreland deformation of Alpine-type orogens
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An alternative view of the Gondwana Paleozoic apparent polar wander path
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Paleomagnetic evidence for tectonic rotation of the Oregon Coast Range
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The Fit of the Southern Continents
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A New Class of Faults and Their Bearing on Continental Drift
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Did the Atlantic Close and then Re-Open?
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Archaean high grade complexes and modern continental margins
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Precambrian and Early Palaeozoic Palaeomagnetism in Australia
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Identifiers
DOI
10.1016/S0166-2635(08)70031-8
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