Barry, T. L.; Ivanov, A. V.; Rasskazov, S. V.; Demonterova, E. I.; Dunai, T. J.; Davies, G. R. and Harrison, D.
|DOI (Digital Object Identifier) Link:||http://doi.org/10.1016/jlithos.2006.09.003|
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Small-volume alkali basaltic volcanism has occurred intermittently for the past +30 My across a vast area of thick continental crust from southern Siberia, through Mongolia to northeast China. With a lack of evidence for large-scale crustal extension or rifting, models to explain the widely dispersed, yet long-lived, volcanism tend to favour involvement of one or more mantle plume(s). We examine the range of 3He/4He isotope values in olivine phenocrysts from basalts, and their entrained mantle xenoliths, from Hamar Daban in southern Siberia, and Hangai in central Mongolia, in order to examine whether upwelling lower mantle appears to be present beneath central Asia and thus test the validity of the plume model for this region. Our results show that the maximum 3He/4He value for the Siberian basalts is 8.12 ± 0.2 Ra, and the maximum value for Mongolian basalts is 9.5 0.5 Ra. These values suggest that there is no significant contribution from a high 3He/4He primordial component that would strongly argue a lower mantle source. Overlap with commonly reported values for MORB, leads us to propose that the source of the magmatism derives from the shallow asthenosphere. Alternative models to a deeply sourced mantle plume, that may be able to explain the magmatism include: a shallow thermal anomaly confined to the upper mantle but fed either laterally or caused by thermal blanketing of the large Asian landmass; replacement or delamination of the lowermost lithosphere in response to tectonic stresses; or large-scale mantle disturbance or overturn caused by a protracted history of subduction beneath central Asia that ended regionally with the Jurassic closure of the Mongol-Okhotsk Ocean, but continues further afield with the present Indo-Asia collision.
|Item Type:||Journal Article|
|Keywords:||Central Asia; Helium isotopes; Continental volcanism; mantle dynamics; mantle plumes|
|Academic Unit/Department:||Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
|Interdisciplinary Research Centre:||Centre for Earth, Planetary, Space and Astronomical Research (CEPSAR)|
|Depositing User:||Tiffany Barry|
|Date Deposited:||28 Jan 2009 06:21|
|Last Modified:||04 Oct 2016 10:07|
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