Results 161 to 170 of about 28,387 (229)
Oxygen isotope composition of Mesoproterozoic (~1360 Ma) seawater constrained by clumped isotopes of North China limestones. [PDF]
Sci AdvLi P +6 more
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Precambrian Research Center Annual Report 2011
, 2012 University of Minnesota Duluth. Precambrian Research Center
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Enhanced metamorphic CO<sub>2</sub> release on the Proterozoic Earth. [PDF]
Proc Natl Acad Sci U S AStewart EM, Penman DE.
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Integrated GIS and AHP framework for groundwater potential mapping in a Himalayan foothill district of Northeast India. [PDF]
Sci RepBasumatary S, Maji S.
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Precambrian Research Center Annual Report 2013
, 2014 University of Minnesota Duluth. Precambrian Research Center
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Precambrian Research Center Annual Report 2012
, 2013 University of Minnesota Duluth. Precambrian Research Center
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Precambrian Research Center Annual Report 2008
, 2009 University of Minnesota Duluth. Precambrian Research Center
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Science, 1981
The Precambrian record is interpreted in terms of an evolutionary progression that moves in the direction of increasing continental stability. An early, highly mobile microplate tectonics phase progressed through a more stable, largely intracratonic, ensialic, mobile belt phase to the modern macroplate tectonics phase that involves large, rigid ...
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The Precambrian record is interpreted in terms of an evolutionary progression that moves in the direction of increasing continental stability. An early, highly mobile microplate tectonics phase progressed through a more stable, largely intracratonic, ensialic, mobile belt phase to the modern macroplate tectonics phase that involves large, rigid ...
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Geological Society, London, Memoirs, 1992
Abstract For much of Precambrian time, it is not possible to reconstruct any sort of meaningful palaeogeographies. For this Atlas, therefore, the earliest reconstructions are for Proterozoic intervals and are, of necessity, limited geographically.
R. Anderton, W. Gibbons, P. G. Nicholson
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Abstract For much of Precambrian time, it is not possible to reconstruct any sort of meaningful palaeogeographies. For this Atlas, therefore, the earliest reconstructions are for Proterozoic intervals and are, of necessity, limited geographically.
R. Anderton, W. Gibbons, P. G. Nicholson
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1982
Abstract Phanerozoic tectonics have not affected the basic integrity of the North American continent. From time to time, sialic crustal elements have been rifted off, accreted onto, and slipped along the continent’s margins, but the vast continental interior has remained intact.
P. F. Hoffman, K. D. Card, A. Davidson
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Abstract Phanerozoic tectonics have not affected the basic integrity of the North American continent. From time to time, sialic crustal elements have been rifted off, accreted onto, and slipped along the continent’s margins, but the vast continental interior has remained intact.
P. F. Hoffman, K. D. Card, A. Davidson
openaire +1 more source