Results 131 to 140 of about 4,715 (162)
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Chemical Geology, 2002
0009-2541/02/$ see front matter D 2002 Elsevier Science B.V. All rights reserved. PII: S0009 -2541 (02 )00012 -8 $ PII of original article S0009-2541(00)00427-7. * Corresponding author. Present address: Laboratoire Magmas et Volcans, CNRS-UMR 6524, Universite Blaise Pascal, 5 rue Kessler, 63038 Clermont-Ferrand, France. Fax: +33-473-346-744.
K. David +5 more
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0009-2541/02/$ see front matter D 2002 Elsevier Science B.V. All rights reserved. PII: S0009 -2541 (02 )00012 -8 $ PII of original article S0009-2541(00)00427-7. * Corresponding author. Present address: Laboratoire Magmas et Volcans, CNRS-UMR 6524, Universite Blaise Pascal, 5 rue Kessler, 63038 Clermont-Ferrand, France. Fax: +33-473-346-744.
K. David +5 more
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Hf isotope compositions of U.S: Geological Survey reference materials. Geochemistry [PDF]
info:eu-repo/semantics ...
Weis, Dominique +8 more
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International Geology Review, 2013
A large mafic dike swarm is radially distributed in southern Qiangtang. Three typical samples were selected for geochronology, geochemistry, and Hf isotopic analysis. Zircon U–Pb dating indicates that the three dikes formed at 291 ± 2, 292 ± 3, and 300 ± 2 Ma.
Ming Wang +3 more
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A large mafic dike swarm is radially distributed in southern Qiangtang. Three typical samples were selected for geochronology, geochemistry, and Hf isotopic analysis. Zircon U–Pb dating indicates that the three dikes formed at 291 ± 2, 292 ± 3, and 300 ± 2 Ma.
Ming Wang +3 more
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Geochimica et Cosmochimica Acta, 2000
Zircon megacrysts represent a late stage in the crystallisation of the magmas that produced the low-Cr megacryst suite (Ol1Opx1Cpx1Gnt1Ilm1Phl1Zir) found in many kimberlites, and may carry information on the sources of the parent magmas and the interaction of these magmas with the cratonic lithosphere.
W.L. Griffin +6 more
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Zircon megacrysts represent a late stage in the crystallisation of the magmas that produced the low-Cr megacryst suite (Ol1Opx1Cpx1Gnt1Ilm1Phl1Zir) found in many kimberlites, and may carry information on the sources of the parent magmas and the interaction of these magmas with the cratonic lithosphere.
W.L. Griffin +6 more
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Precambrian Research, 1996
The Archean Uchi Subprovince, located in the northwestern Superior Province, comprises greenstone belts and granitoid complexes that formed in the course of a multistage history between about 3000 and 2690 Ma. The earliest volcanic-plutonic complexes were assembled into a microcontinent, which then progressively grew by the addition of magmatic arcs ...
F. Corfu, G.M. Stott
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The Archean Uchi Subprovince, located in the northwestern Superior Province, comprises greenstone belts and granitoid complexes that formed in the course of a multistage history between about 3000 and 2690 Ma. The earliest volcanic-plutonic complexes were assembled into a microcontinent, which then progressively grew by the addition of magmatic arcs ...
F. Corfu, G.M. Stott
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Lithos, 2012
Abstract Mesozoic magmatism is extensively developed in eastern China along the eastern Asian continental margin, but the geochronological framework is not well understood for each area. In this study, seventy-eight samples were collected from the Mesozoic igneous rocks in south Anhui Province, east-central China, in order to precisely constrain ...
Fu-Yuan Wu +4 more
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Abstract Mesozoic magmatism is extensively developed in eastern China along the eastern Asian continental margin, but the geochronological framework is not well understood for each area. In this study, seventy-eight samples were collected from the Mesozoic igneous rocks in south Anhui Province, east-central China, in order to precisely constrain ...
Fu-Yuan Wu +4 more
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Chemical Geology, 2017
Abstract Drill core samples from the 3.33 Ga high-alumina-type Commondale komatiites from the southern Kaapvaal craton (South Africa) were analysed for major, trace elements and Hf- isotope compositions in order to place possible constraints on their mantle sources and the process and timing of mantle depletion.
J. Elis Hoffmann, Allan H. Wilson
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Abstract Drill core samples from the 3.33 Ga high-alumina-type Commondale komatiites from the southern Kaapvaal craton (South Africa) were analysed for major, trace elements and Hf- isotope compositions in order to place possible constraints on their mantle sources and the process and timing of mantle depletion.
J. Elis Hoffmann, Allan H. Wilson
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Terra Nova, 2018
AbstractThe Permian Akiyoshi Belt, which is the oldest unmetamorphosed accretionary complex in Southwest Japan, plays an important role in understanding the origin of the Japanese Islands; however, its tectonic affinity is still not well constrained.
Xiaojing Zhang +2 more
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AbstractThe Permian Akiyoshi Belt, which is the oldest unmetamorphosed accretionary complex in Southwest Japan, plays an important role in understanding the origin of the Japanese Islands; however, its tectonic affinity is still not well constrained.
Xiaojing Zhang +2 more
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Geochimica et Cosmochimica Acta, 2002
12th Annual V.M. Goldschmidt Conference Davos Switzerland, The Lu-Hf isotope composition of cratonic lithosphere: disequilibrium between garnet and clinopyroxene in kimberlite xenoliths(DTM, Carnegie Institution of Washington), Pearson, D.G. (University of Durham)
Simon, N.S.C. +3 more
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12th Annual V.M. Goldschmidt Conference Davos Switzerland, The Lu-Hf isotope composition of cratonic lithosphere: disequilibrium between garnet and clinopyroxene in kimberlite xenoliths(DTM, Carnegie Institution of Washington), Pearson, D.G. (University of Durham)
Simon, N.S.C. +3 more
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2005
Morphological and trace element studies of a hundred and twenty-one zircon grains separated from a chlorite–alkali feldspar xenolith of metasomatic origin collected from Valle Guffari (Hyblean Plateau, south-eastern Sicily, Italy) indicated the coexistence of igneous and hydrothermal zircons within the same sample.
SAPIENZA G +4 more
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Morphological and trace element studies of a hundred and twenty-one zircon grains separated from a chlorite–alkali feldspar xenolith of metasomatic origin collected from Valle Guffari (Hyblean Plateau, south-eastern Sicily, Italy) indicated the coexistence of igneous and hydrothermal zircons within the same sample.
SAPIENZA G +4 more
openaire +2 more sources

