Results 221 to 230 of about 31,446 (282)
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Proterozoic stromatolite zonation
American Journal of Science, 1969The zonation of the Proterozoic of the USSR is reviewed and extension to other places is attempted. Preliminary results are: some of the columnar stromatolites of northern Eurasia occur in other continents and in the same stratigraphic ranges; some of the forms (9species9) of the distinctive columnar types have intercontinental distribution, such as ...
P. E. Cloud, M. A. Semikhatov
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Paleobiology, 2005
Abstract A large, morphologically heterogeneous population of acanthomorphic acritarchs from the early Neoproterozoic Wynniatt Formation, Victoria Island, northwestern Canada, is ascribed to two form-genera, Tappania and Germinosphaera, but just a single natural taxon, Tappania. Analysis of Tappania morphology shows it to have been an actively growing,
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Abstract A large, morphologically heterogeneous population of acanthomorphic acritarchs from the early Neoproterozoic Wynniatt Formation, Victoria Island, northwestern Canada, is ascribed to two form-genera, Tappania and Germinosphaera, but just a single natural taxon, Tappania. Analysis of Tappania morphology shows it to have been an actively growing,
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2020
The Indian Subcontinent is comprised of the Archean-Proterozoic cratons, the Aravalli Craton, the Bundelkhand Craton, the Mehghalaya Craton, the Bastar Craton, the Singhbhum Craton and the Dharwar Craton.
A. K. Jain +2 more
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The Indian Subcontinent is comprised of the Archean-Proterozoic cratons, the Aravalli Craton, the Bundelkhand Craton, the Mehghalaya Craton, the Bastar Craton, the Singhbhum Craton and the Dharwar Craton.
A. K. Jain +2 more
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Early Proterozoic climates and plate motions inferred from major element chemistry of lutites
Nature, 1982H. Nesbitt, G. M. Young
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Neodymium isotopes in the Colorado Front Range and crust–mantle evolution in the Proterozoic
Nature, 1981D. DePaolo
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Proterozoic Anorthosite Massifs
1985Major anorthositic massifs intruded stable cratonic crust in the North Atlantic region about 1.4 to 1.7 Ga ago. Similar (meta-) anorthosite massifs (0.9–1.6 Ga) in Grenville and Sveconorwegian terranes exhibit varying degrees of deformational and metamorphic overprint and consequently have ambiguous tectonic settings.
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United Plates of America, The Birth of a Craton: Early Proterozoic Assembly and Growth of Laurentia
, 1988P. Hoffman
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