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Zircon SIMS ages and chemical compositions from Northern Dabie Terrain: Its implication for pyroxenite genesis
Ist Teil von
Chinese science bulletin, 2001-06, Vol.46 (12), p.1047-1050
Ort / Verlag
Department of Earth and Space Sciences, University of Science and Technology of China,%Department of Earth Sciences, Nanjing University,%CRPG-CNRS, Nancy 54501, France
Erscheinungsjahr
2001
Beschreibungen/Notizen
P3; We present the results of a detailed micro-scale investigation of zircons from pyroxenites, Daoshicong Northern Dabie using a combination of SIMS and ICPMS. The SIMS measurements gave ages of 134-159 Ma. Its average of (144.5±6.2) Ma is interpreted as the best estimate of the pyroxenite intrusion. The crystallization of zircons continued for quite a long time and underwent slow cooling. The py-roxenites are products of post-collision magmatism. The REE pattern is HREE-enriched, and its HREE concentra-tions fall between the magmatic and metamorphic range of gneissic zircons from the Dabie area, which indicate the involvement of crust material in its mantle source.
Sprache
Englisch
Identifikatoren
ISSN: 1001-6538
eISSN: 1861-9541
DOI: 10.1007/BF03183556
Titel-ID: cdi_wanfang_journals_kxtb_e200112019
Format
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