Results 161 to 170 of about 5,793 (215)
Juxtaposed slab dehydration, decarbonation and seismotectonic variation beneath the Philippine subduction zone based on 3-D modeling. [PDF]
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Eclogites and Eclogites: Their Differences and Similarities
Geological Society of America Bulletin, 1965Eclogites are divisible into three groups based on mode of occurrence: Group A, inclusions in kimberlites, basalts, or layers in ultramafic rocks; Group B, bands or lenses within migmatite gneissic terrains; Group C, bands or lenses within alpine-type metamorphic rocks.
R. G. COLEMAN +3 more
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Eclogites and eclogites in the Western Gneiss Region, Norwegian Caledonides
Lithos, 2000The Western Gneiss Region WGR marks the outcrop of a composite terrane consisting of variably re-worked Proterozoic basement and parautochthonous or autochthonous cover units. The WGR exhibits a gross structural, petrographic . and thermobarometric zonation from southeast to northwest, reflecting an increasing intensity of Scandian late ...
S.J Cuthbert +3 more
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Eclogites and eclogites: Implications for Archean tectonics
GeologyAbstract Eclogites are generally divided into two types, xenolithic (mantle) and orogenic (crustal). Xenolithic eclogites are late Archean (ca. 3.0−2.5 Ga) or Paleoproterozoic (ca. 2.1−1.7 Ga) in age and are widely interpreted to have been entrained in younger carbonated magmas as they rose through the lithospheric mantle roots of ...
Michael Brown +2 more
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Eclogites and the Eclogite Facies
1965The rock name eclogite was coined by Hauy, a founder of crystallography, in 1822. Since the original definition of the name was vague, its meaning was gradually settled through its usage in later years. According to the generally established usage in the first half of the twentieth century, it means a rock mainly composed of omphacite and almandine ...
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Tectonic significance of Alpine eclogites
Journal of Geodynamics, 1996Abstract A review of P-T peaks and paths of eo- and meso-Alpine eclogite fades rocks occurring along the axial part of the Alpine chain shows that rocks re-equilibrated under high- and low- T (group-B and -C eclogites), are, respectively, hosted within a lower and an upper tectonic level of the Penninic nappe system.
M.I. Spalla +4 more
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Experimental studies on eclogites: The roles of magnetite and acmite in eclogitic assemblages
Chemical Geology, 1968Abstract Reactions between albite, magnetite, garnet and clinopyroxene solid solutions have been studied at pressures up to 36 kbar at 1,100–1,300°C. A low pressure clinopyroxene + magnetite + plagioclase assemblage is replaced by a high pressure clinopyroxene + garnet + magnetite assemblage, or at intermediate pressures and higher temperatures, by a
S Banno, D.H Green
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