Articles | Volume 9, issue 5
https://doi.org/10.5194/se-9-1179-2018
https://doi.org/10.5194/se-9-1179-2018
Research article
 | 
22 Oct 2018
Research article |  | 22 Oct 2018

Permian plume beneath Tarim from receiver functions

Lev Vinnik, Yangfan Deng, Grigoriy Kosarev, Sergey Oreshin, and Larissa Makeyeva

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Yangfan Deng on behalf of the Authors (15 Jul 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (22 Jul 2018) by Caroline Beghein
RR by Rob Porritt (02 Aug 2018)
RR by Jennifer Jenkins (27 Aug 2018)
ED: Reconsider after major revisions (31 Aug 2018) by Caroline Beghein
AR by Yangfan Deng on behalf of the Authors (20 Sep 2018)  Author's response   Manuscript 
ED: Publish as is (01 Oct 2018) by Caroline Beghein
ED: Publish as is (04 Oct 2018) by Federico Rossetti (Executive editor)
AR by Yangfan Deng on behalf of the Authors (06 Oct 2018)  Author's response   Manuscript 
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Short summary
We used seismology data to estimate the thickness of the MTZ and found it thinned beneath Tarim, which is exactly beneath the Permian basalts. This relation can be reconciled with coherent translation of a tectosphere that extends to a depth of 410 km or more. Combined with observations in the Siberian large igneous province and Greenland, these features may confirm the existence of a deep tectosphere. Alternatively, the shift of Tarim is less than predicted by an order of magnitude.