Scientific Quarterly Journal of Geosciences

Scientific Quarterly Journal of Geosciences

Comparison of sedimentology and changes in the sedimentary environment of the Shurijeh Formation in the central and eastern parts of the Kopet-Dagh Basin, northeastern Iran

Document Type : Original Research Paper

Authors
Department of Geology, Faculty of Science, Ferdowsi University of Mashhad, Mashhad, Iran
Abstract
The Shurijeh Formation (Early Cretaceous) in the studied sections in northeastern Iran, with a thickness of 570.40 m in Bid-Sukhteh and 850 m in Radkan, consists of conglomerate, sandstone, shale (mudstone), limestone, and dolomite. A detailed facies analysis indicates the presence of 7 types of coarse-grained facies (Gmm, Gmg, Gci, Gcm, Gh, Gt, Gms), 6 sandstone facies (St, Sp, Sm, Sh, Sl, Sr), 2 fine-grained facies (Fm, Fl), 2 intertidal facies (bioclastic sandy dolomite, dolostone), and 17 diverse subtidal facies. Based on the studied facies, the sedimentary environment of these deposits is primarily continental, characterized by a meandering fluvial system with low sinuosity, and a marine carbonate ramp. Sequence stratigraphic studies have identified 3 sedimentary sequences of third-order in each of the studied sections. Fluctuations in the water table in continental sediments and sea- level changes in marine sediments have resulted in facies diversity in these sections.
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