Boletín de la Sociedad Geológica Mexicana Volumen 75, núm. 2, A070323, 2023 http://dx.doi.org/10.18268/BSGM2023v75n2a070323

Lithostratigraphy, lithofacies and deposition conditions of the late Olenekian-middle Anisian Alam Formation in the Nakhlak area, central Iran

Litoestratigrafía, litofacies y condiciones de depósito de la Formación Alam del Olekiniano tardío-Anisiano medio en el área de Nakhlak, Irán central

Payman Rezaee^1,*, Seyedeh Akram Jooybari¹, Kiamars Hosseini¹, Amin Moodi¹

¹ Department of Geology, University of Hormozgan, Bandar Abbas, Iran.

* Corresponding author: (P. Rezaee) This email address is being protected from spambots. You need JavaScript enabled to view it.

How to cite this article:

Rezaee, P., Jooybari, S.A., Hosseini, K., Moodi, A., 2023, Lithostratigraphy, lithofacies and deposition conditions of the late Olenekian-middle Anisian Alam Formation in the Nakhlak area, central Iran: Boletín de la Sociedad Geológica Mexicana, 75 (2), A070323. http://dx.doi.org/10.18268/BSGM2023v75n2a070323

Manuscript received: July 31, 2022; Corrected manuscript received: January 2, 2023, Manuscript accepted: March 5, 2023.

ABSTRACT

The present study aims to investigate petrography characteristics and sedimental environments of upper Olenekian–middle Anisian deposits of Nakhlak group in the sedimentary-structural zone of central Iran. To this end, a section of these deposits with a thickness of 720 meters was first selected, and 190 samples were taken from this section for preparing thin sections. Also, quantitative and qualitative laboratory tests were performed and 25 samples of sandstone were selected for point counter analysis. The results indicated that the major deposits of this formation are related to siliciclastic, carbonate, and pyroclastic types, which are in the form of two facies associations. The facies association A at the bottom of the studied section with the thickness of 90 meters has a periodicity of clastic, carbonate, and pyroclastic facies. The clastic facies of this association consists of fine-grained sandstone. In addition, the carbonate facies in association A are characterized by two microfacies consisting of intraclast oolitic grainstone and oolitic grainstone. Further, tuffite is the only pyroclastic facies related to association A, which has a laminate structure, cross-bedding lamination, herringbone bedding, and upward-thinning and thickening cycles. The facies association, B which is deposited later, is more in the middle and top part of the section. The facies association B is 660 meters thick and has a periodicity of clastic and limestone facies. Clastic facies of this association includes four lithofacies such as conglomerate, pebble coarse-grained sandstone, medium-grained sandstone to thin layer siltstone and shale. The carbonate facies consists of four microfacies such as sandy intraclastic wackestone and mudstone. Furthermore, slumping structures, cross bedding, turbulence, boudinage structure, and convolute of sediments, along with the effects of erosional channels are observed in facies B. Field and laboratory studies conducted on this succession indicate the structure of facies association A was deposited in a mixed siliciclastic carbonate ramp. Finally, submarine canyons and submarine fan environments were left by increasing the depth of the facies association B in the deep part of sea and turbidity systems.

Keywords: petrography, depositional environments, Upper Olenekian-Anisian, Alam Formation.