Identification of the Oligocene-Miocene boundary in the Central Iran Basin (Qom Formation): Calcareous nannofossil evidences

Authors

  • Mohammad Parandavar Department of Geology, Faculty of Sciences, Ferdowsi University of Mashhad, Mashhad, Iran.
  • Fatemeh Hadavi Department of Geology, Faculty of Sciences, Ferdowsi University of Mashhad, Mashhad, Iran. Email address: fhadavi@um.ac.ir

DOI:

https://doi.org/10.7306/gq.1464

Keywords:

Oligocene-Miocene boundary, Calcareous nannofossil, Biohorizons, Central Iran Basin, Qom Formation, ʺc1ʺ member.

Abstract

A diverse Late Oligocene to Early Miocene calcareous nannofossil assemblage was examined from the Qom Formation in the Central Iran Basin, and the Oligocene-Miocene boundary was identified based on the quantitative analysis of the assemblages in 303 smear slides. Eleven well-established calcareous nannofossil bio-events are delineated in the Upper Oligocene through Lower Miocene. The results clearly show that the Highest Occurrence (HO) of Sphenolithus delphix is the closest bio-event to the boundary as traditionally delineated on the lithostratigraphic criteria, and provides a distinct biohorizon below it. The Lowest Occurrence (LO) of the species Discoaster druggii is the oldest Miocene bio-event that is observed shortly after the HO of S. delphix, showing that calcareous nannofossils are well suited for approximating the Oligocene-Miocene boundary in the Qom Formation. The Oligocene-Miocene boundary is placed in the upper part of Sub-member “c1” in all three sections studied here and it is traceable throughout the Central Iran Basin, which makes a potentially reliable marker horizon for sequence stratigraphic and hydrocarbon studies in the area.

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Published

2019-07-10

Issue

Vol. 63 No. 2 (2019)

Section

Articles

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