Forward propagation of the Zagros Simply Folded Belt constrained from magnetostratigraphy of growth strata

• Published in: Tectonics (Washington, D.C.) Vol. 33; no. 8; pp. 1534 - 1551
• Main Authors: Ruh, Jonas B., Hirt, Ann M., Burg, Jean-Pierre, Mohammadi, Ali
• Format: Journal Article
• Language: English
• Published: Washington Blackwell Publishing Ltd 01-08-2014
• Subjects: Alluvial rivers; Conglomerates; Fluvial sediments; growth strata; magnetostratigraphy; Miocene; Plate tectonics; Propagation; Sedimentation & deposition; Seismology; Simply Folded Belt; Stratigraphy; Unconformity; Zagros
• ISSN: 0278-7407; 1944-9194
• DOI: 10.1002/2013TC003465

The temporal evolution of the Zagros Simply Folded Belt is constrained by a magnetostratigraphic sequence containing a progressive unconformity on the southern limb of the Kuh‐e Ghol Ghol anticline, in the Central Fars. The investigated ~1400 m thick sequence exposes a regressive megacycle containing, from bottom to top, open and shallow marine marls and sandy limestones, fine‐ to coarse‐grained fluvial deposits and alluvial conglomerates. Correlating the magnetostratigraphic section with the geomagnetic polarity time scale constrains the transition from marine to fluvial sediment deposition at ~6 Ma. This transition was accompanied by a change in the accumulation rate from ~15 cm/ka to ~40 cm/ka, as measured on lithified sediments. Alluvial river deposits first occurred at ~3.2 Ma. The Kuh‐e Ghol Ghol anticline began to grow at ~3.8 Ma, witnessing fastest limb rotation rates of 40°/Ma at ~3.3 Ma. Reporting magnetostratigraphic sections and ages of growth strata on a map of NE Fars reveal an ~1 cm/a, southwestward migration rate of the deformation front during the middle and late Miocene.
Key Points
Growth strata indicate syntectonic sedimentation processes in the ZagrosGrowth strata were dated by magnetostratigraphy in the Central FarsFolds in the Central Fars started to grow at 3.8 Ma