Articles | Volume 9, issue 6
https://doi.org/10.5194/se-9-1375-2018
https://doi.org/10.5194/se-9-1375-2018
Research article
 | 
29 Nov 2018
Research article |  | 29 Nov 2018

New insights on the early Mesozoic evolution of multiple tectonic regimes in the northeastern North China Craton from the detrital zircon provenance of sedimentary strata

Yi Ni Wang, Wen Liang Xu, Feng Wang, and Xiao Bo Li

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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 Wen Liang Xu on behalf of the Authors (07 Oct 2018)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (19 Oct 2018) by Federico Rossetti
RR by Anonymous Referee #1 (28 Oct 2018)
ED: Publish subject to minor revisions (review by editor) (29 Oct 2018) by Federico Rossetti
AR by Wen Liang Xu on behalf of the Authors (02 Nov 2018)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (02 Nov 2018) by Federico Rossetti
AR by Wen Liang Xu on behalf of the Authors (09 Nov 2018)  Author's response   Manuscript 
ED: Publish subject to technical corrections (16 Nov 2018) by Federico Rossetti
ED: Publish subject to technical corrections (16 Nov 2018) by Federico Rossetti (Executive editor)
AR by Wen Liang Xu on behalf of the Authors (18 Nov 2018)  Author's response   Manuscript 
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Short summary
Early Triassic sediments in the northeastern North Chian Craton resulted from the subduction of the Paleo-Asian oceanic plate and collision between the North China and Yangtze cratons. Late Triassic sediments resulted from the final closure of the Paleo-Asian Ocean in the Middle Triassic and exhumation of the Su–Lu Orogenic Belt. Early Jurassic change in provenance was related to the uplift of the Xing'an–Mongolia Orogenic Belt and the subduction of the Paleo-Pacific Plate.