Results 251 to 260 of about 144,129 (292)

Buried, not erased: palynofloras in ultra-high-pressure metamorphic rocks. [PDF]

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Carosi R   +6 more
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Tectonics and Evolution of Venus

Science, 1981
The global tectonics of Venus differs significantly from that of Earth, most markedly in that the surface is covered predominately by gently rolling terrain; there apparently are no features like ocean rises; the gravity is positively correlated with topography at all wavelengths; and the few highlands are estimated to be supported or compensated at a ...
R J, Phillips   +3 more
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Tectonic evolution of Mars

Journal of Geophysical Research: Solid Earth, 1979
Any model for the tectonic evolution of Mars must account for two major crustal elements: the Tharsis bulge and the topographically low and lightly cratered northern third of the planet. Ages determined by crater density indicate that both of these elements came into existence very early in Martian history, a conclusion that holds no matter which of ...
Donald U. Wise   +2 more
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Chapter 14 Tectonic Evolution

Geological Society, London, Memoirs, 2005
The concept that SE Asia, and indeed Asia as a whole, has been built up during the Phanerozoic by the amalgamation of allochthonous terranes derived from the northern margin of East Gondwana, is now well established in the literature (e.g. Audley-Charles 1988; Sengor et al .
A. J. Barber   +2 more
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TECTONIC EVOLUTION OF ALTAIDES

Russian Geology and Geophysics, 1994
A model is proposed according to which the Paleozoic folded structures of Tien Shan, Kazakhstan, Altai, and Mongolia framing the Angarian, or Siberian, cratons and forming an orogenic collage of Altaides could originate along a single subduction boundary consisting of the Tuva-Mongolian and Kipchak arcs. As a result of the Vendian-Cambrian rifting, the
A. M. C. Şengör   +2 more
openaire   +1 more source

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