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- W2364195414 abstract "The Luobusha ophiolite consisting of a complete ophiolite sequences,is located in the eastern segment of the Yarlung Zangpo suture zone. It is characterized by the occurrence of the strongly deformed mantle peridotites,obduction type plagiogranites in the upper part of the cumulate sequence,diabasic dikes intruded the peridotites; and thin complicated crustal lavas. Isotopic study of the Luobusha peridotites reveals that the rocks are characterized by high initial 87Sr/86Sr (0.705489~0.714625),low initial 143Nd/144Nd (0.511796~0.512605) ratios and variabale eNd(t) values,which are similar to those of EMI. The high Δ7/4Pb and Δ8/4Pb values exhibit a source with Dupal anomaly. Considering the known regional tectonic evolution,the Luobusha ophiolitic peridotites should have been formed under the influence of a mantle plume that assimilated sediments from subducted slab." @default.
- W2364195414 created "2016-06-24" @default.
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- W2364195414 date "2011-01-01" @default.
- W2364195414 modified "2023-09-25" @default.
- W2364195414 title "Sr-Nd-Pb Isotopic Characteristics and Origin of the Mantle Peridotites from the Luobusha Ophiolite" @default.
- W2364195414 hasPublicationYear "2011" @default.
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