MORB-type rocks from the Paleo-Tethyan Mian-Lueyang northern ophiolite in the Qinling Mountains, central China: implications for the source of the low 206Pb/204Pb and high 143Nd/144Nd mantle component in the Indian Ocean

Details MORB-type rocks from the Paleo-Tethyan Mian-Lueyang northern ophiolite in the Qinling Mountains, central China: implications for the source of the low 206Pb/204Pb and high 143Nd/144Nd mantle component in the Indian Ocean MORB-type rocks from the Paleo-Tethyan Mian-Lueyang northern ophiolite in the Qinling Mountains, central China: implications for the source of the low 206Pb/204Pb and high 143Nd/144Nd mantle component in the Indian Ocean

May 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002e%26psl.198..323x&link_type=abstract

Earth and Planetary Science Letters, Volume 198, Issue 3-4, p. 323-337.

Computer Science

8

Scientific paper

Samples from a basalt and gabbro section of the Paleo-Tethyan (~350 Ma) Mian-Lue northern ophiolites (MLNO) in the Qinling Mountains of central China display sub-parallel and relatively smooth incompatible trace element-depleted patterns and have high ɛNd(350 Ma) (8.1-11.3) and low 206Pb/204Pb(350 Ma) (16.90-17.25). The MLNO basalts and gabbros are compositionally similar to normal mid-ocean ridge basalts (MORB), particularly to those from the Carlsberg Ridge and Indian Ocean Ridge Triple Junction. The basalts and gabbros also have high Δ7/4 and Δ8/4 isotopic values characteristic of the Dupal isotopic anomaly in the southern hemisphere. Although the MLNO is presently in the northern hemisphere, it was previously located within the southerly location of the Indian Ocean based on paleomagnetic data. Thus, assuming that the low 206Pb/204Pb ratio of the MLNO basalts and gabbros is not due to seawater alteration or continental contamination, the unique isotopic signature of both the Paleo-Tethyan oceanic igneous crust and the modern Indian MORB may have come from a very similar, if not identical mantle reservoir. This indicates that a portion of the modern Indian MORB mantle isotopic domain could have been in existence for at least ~350 Ma. We propose that the low 206Pb/204Pb and high 143Nd/144Nd isotopic character of the MLNO basalts and gabbros as well as similar Indian MORB originated either from a low μ sub-domain of the depleted asthenospheric mantle in the southern hemisphere or due to contamination of the depleted asthenosphere by deep-rooted plumes carrying a low 206Pb/204Pb mantle component. In contrast, the origin of the more common Indian MORB with low 206Pb/204Pb and low 143Nd/144Nd is most probably associated with the delamination of the Gondwanan continental lithosphere during formation of the Indian Ocean.

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