Journal cover Journal topic
Earth Surface Dynamics An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 3.765 IF 3.765
  • IF 5-year value: 3.719 IF 5-year
    3.719
  • CiteScore value: 3.83 CiteScore
    3.83
  • SNIP value: 1.281 SNIP 1.281
  • IPP value: 3.61 IPP 3.61
  • SJR value: 1.527 SJR 1.527
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 17 Scimago H
    index 17
  • h5-index value: 18 h5-index 18
ESurf | Articles | Volume 7, issue 1
Earth Surf. Dynam., 7, 321-344, 2019
https://doi.org/10.5194/esurf-7-321-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Earth Surf. Dynam., 7, 321-344, 2019
https://doi.org/10.5194/esurf-7-321-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 26 Mar 2019

Research article | 26 Mar 2019

Dating and morpho-stratigraphy of uplifted marine terraces in the Makran subduction zone (Iran)

Raphaël Normand et al.
Download
Interactive discussion
Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Raphaël Normand on behalf of the Authors (30 Jan 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (04 Feb 2019) by Simon Mudd
RR by Vincent Regard (06 Feb 2019)
RR by Julius Jara Muñoz (26 Feb 2019)
ED: Publish subject to technical corrections (28 Feb 2019) by Simon Mudd
ED: Publish subject to technical corrections (28 Feb 2019) by Andreas Lang(Editor)
Publications Copernicus
Download
Short summary
We studied and mapped uplifted marine terraces in southern Iran that are part of the Makran subduction zone. Our results show that most exposed terraces were formed in the last 35 000–250 000 years. Based on their altitude and the paleo sea-level, we derive surface uplift rates of 0.05–5 mm yr−1. The marine terraces, tilted with a short wavelength of 20–30 km, indicate a heterogeneous accumulation of deformation in the overriding plate.
We studied and mapped uplifted marine terraces in southern Iran that are part of the Makran...
Citation