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2183 Creator 1c5c32b11b5ad1bd9c846a77784abc38
2183 Creator ext-190a12e0d9e58b6a57bbb86b783cb1c2
2183 Creator ext-3dd9efcc6eccc280bde9427510148136
2183 Creator ext-4deb0d93da0cc3dfe34c1dfce59e7b1f
2183 Creator ext-56c368bb643874b3193c229556d0248e
2183 Creator ext-8d2102bc6e7254b949da48c5fd33db8f
2183 Creator ext-c6e1a14ef563f3749b1d2849b1ebdbcc
2183 Creator ext-de83224f5512445cc1632248a249cee6
2183 Date 2003
2183 Is Part Of p00107999
2183 Is Part Of repository
2183 abstract Mantle xenoliths from the Obnazhennaya kimberlite pipe, Yakutia, possess a large range of mineralogical and chemical compositions, from both group A and B eclogites. Major-element contents of the group A eclogites exhibit transitional features between the group B eclogites and peridotite. The Mg# of clinopyroxenes is 0.86–0.94, with 0.60–0.84 for garnets. Differences in concentration of LREEs exist between the Obnazhennaya group A and the well-studied group B eclogites from the Udachnaya kimberlite pipe. In general, garnets in the group A eclogites contain lower LREEs than those from the group B eclogites; however, the trend for clinopyroxene is reversed. High d 18O (5.46–7.81) values, and the positive Eu anomalies in the garnets and clinopyroxenes (Eu/Eu* 1.2–1.4) demonstrate the involvement of an oceanic crustal component in the formation of the group A eclogites. The group A eclogites formed between 21.0 and 37.6 kbar, and 711 and 923 °C, in a time interval of 1,071–1,237 Ma. An innovative model is proposed to explain the formation of the group A eclogites and websterites. It involves the reaction of a depleted mantle peridotite with TTG and carbonatite melts closely related to the subduction of oceanic crust.
2183 authorList authors
2183 issue 4
2183 status peerReviewed
2183 volume 145
2183 type AcademicArticle
2183 type Article
2183 label Taylor, Lawrence A.; Snyder, Gregory A.; Keller, Randall; Remley, David A.; Anand, Mahesh ; Wiesli, Rene; Valley, John and Sobolev, Nikolai V. (2003). Petrogenesis of group A eclogites and websterites: evidence from the Obnazhennaya kimberlite, Yakutia. Contributions to Mineralogy and Petrology, 145(4) pp. 424–443.
2183 label Taylor, Lawrence A.; Snyder, Gregory A.; Keller, Randall; Remley, David A.; Anand, Mahesh ; Wiesli, Rene; Valley, John and Sobolev, Nikolai V. (2003). Petrogenesis of group A eclogites and websterites: evidence from the Obnazhennaya kimberlite, Yakutia. Contributions to Mineralogy and Petrology, 145(4) pp. 424–443.
2183 Title Petrogenesis of group A eclogites and websterites: evidence from the Obnazhennaya kimberlite, Yakutia
2183 in dataset oro