1-s2.0-S1342937X19302709-main.pdf (6.51 MB)

Evidence for southward subduction of the Mongol-Okhotsk oceanic plate: Implications from Mesozoic adakitic lavas from Mongolia

Download (6.51 MB)
journal contribution
posted on 02.12.2019, 11:37 by Thomas .C Sheldrick, Tiffany L. Barry, Ian Millar, Dan N. Barfod, Alison M. Halton, Dan J. Smith
A combination of new 40Ar/39Ar dating results, major- and trace-element data, plus Sr-Nd-Pb-Hf isotope data, are used to investigate the petrogenesis of Triassic high-Si adakite (HSA), Cretaceous low-Si adakite-like (LSA) lavas, and Cretaceous high-K and shoshonitic trachyandesite lavas, from eastern and south-central Mongolia. All samples are light rare-earth element and large-ion lithophile element enriched but depleted in some high-field strength elements (notably Nb, Ta and Ti). Two alternative models are proposed to explain the petrogenesis of the HSA samples. (1) A southward-subducting Mongol-Okhotsk slab underwent partial melting in the Triassic during the closure of the Mongol-Okhotsk Ocean, with the resultant melts assimilating mantle and crustal material. Alternatively (2), a basaltic underplate of thickened (>50 km; >1.5 GPa), eclogitic lower crust foundered into the underlying mantle, and underwent partial melting with minor contamination from mantle material and some shallow-level crustal contamination. The LSA samples are interpreted as melts derived from a lithospheric mantle wedge that was previously metasomatised by slab melts. Similarly, the trachyandesite lavas are interpreted as melts deriving from a subduction-enriched subcontinental lithospheric mantle. The spatial distribution of these samples implies that metasomatism likely occurred due to a southward-subducting Mongol-Okhotsk slab associated with the closure of the Mongol-Okhotsk Ocean. When this interpretation is combined with previous evidence for a northward-subducting Mongol-Okhotsk slab it advocates that the Mongol-Okhotsk Ocean closed with double-sided subduction.

Funding

The analyses were supported by NERC grant IP-1610-0516. Thanks to Mungunshagai for providing field assistance.

History

Citation

Gondwana Research, 2020, 79, pp. 140-156

Author affiliation

/Organisation/COLLEGE OF SCIENCE AND ENGINEERING/School of Geography, Geology and the Environment

Version

VoR (Version of Record)

Published in

Gondwana Research

Volume

79

Pagination

140-156

Publisher

Elsevier for International Association for Gondwana Research

issn

1342-937X

Acceptance date

06/09/2019

Copyright date

2019

Available date

17/10/2019

Publisher version

https://www.sciencedirect.com/science/article/pii/S1342937X19302709?via=ihub

Language

en

Licence

Exports