Distinct mantle sources of low-Ti and high-Ti basalts from the western Emeishan large igneous province, SW China: implications for plume lithosphere interaction

Details Distinct mantle sources of low-Ti and high-Ti basalts from the western Emeishan large igneous province, SW China: implications for plume lithosphere interaction Distinct mantle sources of low-Ti and high-Ti basalts from the western Emeishan large igneous province, SW China: implications for plume lithosphere interaction

Dec 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004e%26psl.228..525x&link_type=abstract

Earth and Planetary Science Letters, Volume 228, Issue 3-4, p. 525-546.

Computer Science

16

Emeishan, Sw China, High-Ti And Low-Ti Basalts, Petrogenesis, Mantle Plume, Lithosphere

Scientific paper

The Late Permian Emeishan large igneous province (ELIP), with an areal extent of over 500,000 km2, at the western margin of Yangtze craton, is increasingly regarded as the result of the impingement of a mantle plume onto the lithosphere. However, petrogenesis of the continental flood basalt remains controversial. The best-exposed lava succession in the western ELIP is studied in order to further constrain their petrogenesis and plume lithosphere interaction. The basaltic lava flows of the ELIP are geochemically classified into low-Ti (LT) and high-Ti (HT) types. The LT type lavas exhibit low Ti/Y (<500) and ɛNd(t) (-0.34˜-3.76) but comparatively high Mg# (44 67) and (87Sr/86Sr)i (0.705 0.708), whereas the HT type lavas have high Ti/Y (>500), ɛNd(t) (-1.17˜0.43) but lower Mg# (31 53) and (87Sr/86Sr)i (0.705 0706). The LT basalts can be further subdivided into: LT1 and LT2. LT1 lavas exhibit relatively higher Mg# (51 67) and (87Sr/86Sr)i ratio (0.706 0.707), lower Nb/La ratio (<0.9) and initial ɛNd(t) (-6.74˜-0.34) than the LT2 type lavas (Nb/La>1.1; ɛNd(t)=-1.17˜0.43). Detailed stratigraphic work indicates that there was a temporal progression from LT1 to LT2 to HT-type magmas. This compositional shift cannot be explained simply in terms of a declining extent of crustal contamination of a mantle-derived melt with time. Instead, it seems that the LT and HT type magmas originated from distinct mantle sources and parental magmas. Geochemical features of the early stage LT1 lavas are indicative of a significant contribution from the enriched continental lithosphere mantle, whereas the compositional shift from LT1 to LT2 reveals a trend from predominantly shallower lithospheric mantle to deeper mantle with time. Late stage HT magma formed from a deeper mantle source that may possibly be a mantle plume.

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