Boletín de la Sociedad Geológica Mexicana Volumen 74, núm. 2, A240322, 2022 http://dx.doi.org/10.18268/BSGM2022v74n2a240322

Microbiostratigraphy, microfacies analysis and lateral basin evolution of Lower Cretaceous deposits in the south of Kerman region, SE Iran

Microbioestratigrafía, análisis de microfacies y evolución lateral de la cuenca de los depósitos del Cretácico Inferior en la región sur de Kerman, SE Irán

Mohammad Javad Hassani^1,*

¹ Department of Ecology, Institute of Science and High Technology and Environmental Sciences, Graduate University of Advanced Technology, End of Haft Bagh Highway, Kerman, Iran.

*Corresponding author: (M.J. Hassani) This email address is being protected from spambots. You need JavaScript enabled to view it. , This email address is being protected from spambots. You need JavaScript enabled to view it.

How to cite this article:

Hassani, M.J., Microbiostratigraphy, microfacies analysis and lateral basin evolution of Lower Cretaceous deposits in the south of Kerman region, SE Iran: Boletín de la Sociedad Geológica Mexicana, 74 (2), A240322. http://dx.doi.org/10.18268/BSGM2022v74n2a240322

Manuscript received: February 7, 2022; Corrected manuscript received: March 10, 2022; Manuscript accepted: March 23, 2022.

ABSTRACT

Detailed microbiostratigraphy and basin evolution of the Lower Cretaceous deposits in the Rayen area, south of Kerman Region, SE Iran are investigated for the first time in two sections. The section no. 1 is 324.6m in thickness and comprises five lithostratigraphic units. The section no. 2 is 218 m in thickness and includes three lithostratigraphic units. The identified fauna and flora include 41 benthic foraminifera and 11 calcareous algae species. The identified assemblage indicates that the marine strata in both sections were deposited during the Barremian to Albian. The microfacies analyses carried out on 22 carbonate and 2 clastic microfacies indicate that the deposits in the section no. 1 were deposited on a homoclinal carbonate ramp, whereas in the section no. 2 they were deposited on a rimmed carbonate shelf. Generally, the Cretaceous deposit in the two studied sections represent different sedimentary models and fossil content indicating different basin evolution histories. The paleogeographic setting of the studied area on the south eastern margin of the Central-East Iranian Microcontinent and the active tectonic history during the Mesozoic suggest that the syndepositional tectonism influenced the basement’s morphology and resulted in changes in the fossil diversity and sedimentary nature of adjacent sedimentary basins.

Keywords: Lower Cretaceous, CEIM, basin evolution, Kerman, Rayen.