The influence of hybrid sediment gravity flows on distribution and composition of trace‐fossil assemblages: Ordovician succession of the north‐eastern Alborz Range of Iran-Reference-Cited by-同舟云学术

The influence of hybrid sediment gravity flows on distribution and composition of trace‐fossil assemblages: Ordovician succession of the north‐eastern Alborz Range of Iran

Published:2022-12-28 Issue:3 Volume:70 Page:783-827
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Bayet‐Goll Aram¹^ORCID,Sharafi Mahmoud²^ORCID,Daraei Mehdi¹^ORCID,Nasiri Yaghub³

Affiliation:

1. Department of Earth Sciences Institute for Advanced Studies in Basic Sciences (IASBS) P.O. Box 45195‐1159 Zanjan Iran

2. Department of Geology, Faculty of Science University of Hormozgan P.O. Box 3995 Bandar Abbas Iran

3. Department of Geology, Faculty of Science University of Gonabad P.O. Box 96919‐57678 Gonabad Iran

Funder

Institute for Advanced Studies in Basic Sciences

Publisher

Wiley

Subject

Stratigraphy,Geology,General Medicine

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.13058

Reference107 articles.

1. Tectonostratigraphic synthesis and structural style of the alborz mountain system in Northern Iran

2. Stratigraphic and volcanic signatures of Miaolingian-Late Ordovician rift pulses in the Alborz Mountains, northern Iran

3. Anatomy of turbidites and linked debrites based on long distance (120 x 30 km) bed correlation, Marnoso Arenacea Formation, Northern Apennines, Italy

4. Depositional processes, bedform development and hybrid bed formation in rapidly decelerated cohesive (mud-sand) sediment flows

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