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Lithostratigraphic and Biostratigraphic studies of Neyzar Formation in Jalil- Abad section (northwest of Mashhad, Iran)

Author:
محمد وحیدی نیا
,
Abas Sadeghi
,
Mohammad Vahidinia
Year
: 2011
Abstract: Kopet_ Dagh mountains with NW- SE trend is located in north and northeast of Iran. One of the most formations of Kopet- Dagh basin is Neyzar Formation with Upper Cretaceous age. Studied section located in southern flank of Kalat-e-Naderi syncline, 141 km northwest of Mashhad and adjacent of Kalat-e-Naderi city.

The thickness of Neyzar Formation 555.5 meter was measured. Based on morphological and petrographic characteristics divided to 8 units.

The lower contact of Neyzar Formation with Abtalkh Formation is conformable and the upper contact this formation with Kalat Formation is Disconformable (as a paleosol). At the first time, on the base of Micropaleontological studies, 33 species belonging to 26 genera of Planktonic and Benthonic foraminifer have been reported.

Based on fossils identified especially, Siderolites calcitrapoides, Abathomphalus mayaroensis, Orbitoides apiculata, Orbitoides media, Maaastrichtian especially Late Maastrichtian age for Neyzar Formation have been determined. According to recognized facies, the Neyzar Formation in a Carbonate platform (Ramp type with Bar Islands) has been deposited
URI: https://libsearch.um.ac.ir:443/fum/handle/fum/3379285
Keyword(s): Kopet- Dagh,Neyzar Formation,Paleosol,Planktonic and Benthonic foraminifera,Maastrichtian
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    Lithostratigraphic and Biostratigraphic studies of Neyzar Formation in Jalil- Abad section (northwest of Mashhad, Iran)

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contributor authorمحمد وحیدی نیاen
contributor authorAbas Sadeghien
contributor authorMohammad Vahidiniafa
date accessioned2020-06-06T14:01:30Z
date available2020-06-06T14:01:30Z
date copyright4/25/2011
date issued2011
identifier urihttps://libsearch.um.ac.ir:443/fum/handle/fum/3379285
description abstractKopet_ Dagh mountains with NW- SE trend is located in north and northeast of Iran. One of the most formations of Kopet- Dagh basin is Neyzar Formation with Upper Cretaceous age. Studied section located in southern flank of Kalat-e-Naderi syncline, 141 km northwest of Mashhad and adjacent of Kalat-e-Naderi city.

The thickness of Neyzar Formation 555.5 meter was measured. Based on morphological and petrographic characteristics divided to 8 units.

The lower contact of Neyzar Formation with Abtalkh Formation is conformable and the upper contact this formation with Kalat Formation is Disconformable (as a paleosol). At the first time, on the base of Micropaleontological studies, 33 species belonging to 26 genera of Planktonic and Benthonic foraminifer have been reported.

Based on fossils identified especially, Siderolites calcitrapoides, Abathomphalus mayaroensis, Orbitoides apiculata, Orbitoides media, Maaastrichtian especially Late Maastrichtian age for Neyzar Formation have been determined. According to recognized facies, the Neyzar Formation in a Carbonate platform (Ramp type with Bar Islands) has been deposited
en
languageEnglish
titleLithostratigraphic and Biostratigraphic studies of Neyzar Formation in Jalil- Abad section (northwest of Mashhad, Iran)en
typeConference Paper
contenttypeExternal Fulltext
subject keywordsKopet- Daghen
subject keywordsNeyzar Formationen
subject keywordsPaleosolen
subject keywordsPlanktonic and Benthonic foraminiferaen
subject keywordsMaastrichtianen
identifier linkhttps://profdoc.um.ac.ir/paper-abstract-1021401.html
conference title64th Geologi Congress of Turkeyen
conference locationآنکاراfa
identifier articleid1021401
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