Triggers and sources of volatile-bearing plumes in the mantle transition zone

The paper discusses generation of volatile-bearing plumes in the mantle transition zone (MTZ) in terms of mineral-fluid petrology and their related formation of numerous localities of intra-plate bimodal volcanic series in Central and East Asia. The plume generation in the MTZ can be triggered by th...

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Main Authors: Inna Safonova, Konstantin Litasov, Shigenori Maruyama
Format: Article
Language:English
Published: Elsevier 2015-09-01
Series:Geoscience Frontiers
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674987114001571
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author Inna Safonova
Konstantin Litasov
Shigenori Maruyama
author_facet Inna Safonova
Konstantin Litasov
Shigenori Maruyama
author_sort Inna Safonova
collection DOAJ
description The paper discusses generation of volatile-bearing plumes in the mantle transition zone (MTZ) in terms of mineral-fluid petrology and their related formation of numerous localities of intra-plate bimodal volcanic series in Central and East Asia. The plume generation in the MTZ can be triggered by the tectonic erosion of continental crust at Pacific-type convergent margins and by the presence of water and carbon dioxide in the mantle. Most probable sources of volatiles are the hydrated/carbonated sediments and basalts and serpentinite of oceanic slabs, which can be subducted down to the deep mantle. Tectonic erosion of continental crust supplies crustal material enriched in uranium and thorium into the mantle, which can serve source of heat in the MTZ. The heating in the MTZ induces melting of subducted slabs and continental crust and mantle upwelling, to produce OIB-type mafic and felsic melts, respectively.
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spelling doaj.art-b166870d508f4599ba5321950558524b2023-09-03T00:06:38ZengElsevierGeoscience Frontiers1674-98712015-09-016567968510.1016/j.gsf.2014.11.004Triggers and sources of volatile-bearing plumes in the mantle transition zoneInna Safonova0Konstantin Litasov1Shigenori Maruyama2V.S. Sobolev Institute of Geology and Mineralogy SB RAS, Novosibirsk, RussiaV.S. Sobolev Institute of Geology and Mineralogy SB RAS, Novosibirsk, RussiaEarth-Life Science Institute, Tokyo Institute of Technology, Tokyo, JapanThe paper discusses generation of volatile-bearing plumes in the mantle transition zone (MTZ) in terms of mineral-fluid petrology and their related formation of numerous localities of intra-plate bimodal volcanic series in Central and East Asia. The plume generation in the MTZ can be triggered by the tectonic erosion of continental crust at Pacific-type convergent margins and by the presence of water and carbon dioxide in the mantle. Most probable sources of volatiles are the hydrated/carbonated sediments and basalts and serpentinite of oceanic slabs, which can be subducted down to the deep mantle. Tectonic erosion of continental crust supplies crustal material enriched in uranium and thorium into the mantle, which can serve source of heat in the MTZ. The heating in the MTZ induces melting of subducted slabs and continental crust and mantle upwelling, to produce OIB-type mafic and felsic melts, respectively.http://www.sciencedirect.com/science/article/pii/S1674987114001571AsiaPacific-type convergent marginContinental crust materialHydrated/carbonated oceanic crustSubductionMelting
spellingShingle Inna Safonova
Konstantin Litasov
Shigenori Maruyama
Triggers and sources of volatile-bearing plumes in the mantle transition zone
Geoscience Frontiers
Asia
Pacific-type convergent margin
Continental crust material
Hydrated/carbonated oceanic crust
Subduction
Melting
title Triggers and sources of volatile-bearing plumes in the mantle transition zone
title_full Triggers and sources of volatile-bearing plumes in the mantle transition zone
title_fullStr Triggers and sources of volatile-bearing plumes in the mantle transition zone
title_full_unstemmed Triggers and sources of volatile-bearing plumes in the mantle transition zone
title_short Triggers and sources of volatile-bearing plumes in the mantle transition zone
title_sort triggers and sources of volatile bearing plumes in the mantle transition zone
topic Asia
Pacific-type convergent margin
Continental crust material
Hydrated/carbonated oceanic crust
Subduction
Melting
url http://www.sciencedirect.com/science/article/pii/S1674987114001571
work_keys_str_mv AT innasafonova triggersandsourcesofvolatilebearingplumesinthemantletransitionzone
AT konstantinlitasov triggersandsourcesofvolatilebearingplumesinthemantletransitionzone
AT shigenorimaruyama triggersandsourcesofvolatilebearingplumesinthemantletransitionzone