Abstract
The Quaternary to recent travertines in the Badab-e Surt Spring are distinguished in four lithofacies according to the field and microscopic features. The various recognized lithofacies of travertine deposits include (1) crystalline crust, (2) pisoids, (3) tufa, and (4) carbonate black muds. Various combinations of the distinguished lithofacies are deposited on slope, depression, and mound environments. Mud facies was analyzed using scanning electron microscope (SEM) /energy-dispersive spectrometer (EDS) and represent gypsum and halite crystals. Mechanical CO2 outgassing is the main factor controlling calcite precipitation on the cascades.
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Acknowledgments
The authors thank Mr. Rezae for providing the center of SEM of the University of Tarbiat Modares. We would like to extend our appreciation to our colleagues from the University of Tehran for their assistance with the field work. We would like to thank the Tehran University (School of Geology) for providing financial support.
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Sotohian, F., Ranjbaran, M. Depositional system and facies analysis of travertine deposits: Badab-e Surt Spring Mazandaran, Iran. Arab J Geosci 8, 4939–4947 (2015). https://doi.org/10.1007/s12517-014-1544-2
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DOI: https://doi.org/10.1007/s12517-014-1544-2