NANO STRATIGRAPHY AND SEDIMENTOLOGY OF THE ABDERAZ FORMATION AT SHEIKH SECTION (WESTERN KOPET-DAGH BASIN)

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MOHEGHY M.A.; HADAVI F.

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Journal: JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY) Year:2012 | Volume:8 | Issue:2 Page(s): 159-172

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Title

NANO STRATIGRAPHY AND SEDIMENTOLOGY OF THE ABDERAZ FORMATION AT SHEIKH SECTION (WESTERN KOPET-DAGH BASIN)

Author(s)

MOHEGHY M.A. | HADAVI F. | Issue Writer Certificate

Keywords

BIOZONEQ2

LATE CAMPANIANQ2

EARLY CAMPANIANQ2

CALCAREOUS NANOFOSSILQ1

Abstract

Calcareous nanofossils in the Abderaz Formation at Sheikh Section have been studied. This section is situated in the western part of the Kopet-Dagh Basin. In this study 34 nanoplankton species of 21 genera were identified. According to the first occurrence of index species and fossil assemblages CALCAREOUS NANOFOSSIL BIOZONEs (CC18-CC21) of Sissingh (1997) have been recognized. Based on these BIOZONEs, the age of this formation is EARLY CAMPANIAN-Early LATE CAMPANIAN. The investigation of mentioned nanofossils shows that Abderaz basin at Sheikh Section was deposited in relatively low latitude, relatively high temperature and low productivity so that the depth of the basin to the Kalat Formation increased.

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APA: Copy

MOHEGHY, M.A., & HADAVI, F.. (2012). NANO STRATIGRAPHY AND SEDIMENTOLOGY OF THE ABDERAZ FORMATION AT SHEIKH SECTION (WESTERN KOPET-DAGH BASIN). JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), 8(2), 159-172. SID. https://sid.ir/paper/127116/en

Vancouver: Copy

MOHEGHY M.A., HADAVI F.. NANO STRATIGRAPHY AND SEDIMENTOLOGY OF THE ABDERAZ FORMATION AT SHEIKH SECTION (WESTERN KOPET-DAGH BASIN). JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY)[Internet]. 2012;8(2):159-172. Available from: https://sid.ir/paper/127116/en

IEEE: Copy

M.A. MOHEGHY, and F. HADAVI, “NANO STRATIGRAPHY AND SEDIMENTOLOGY OF THE ABDERAZ FORMATION AT SHEIKH SECTION (WESTERN KOPET-DAGH BASIN),” JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), vol. 8, no. 2, pp. 159–172, 2012, [Online]. Available: https://sid.ir/paper/127116/en

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