Stratigraphy and sedimentology of the avroman formation (Triassic)‎ northeastern Iraq

Other Title(s)

طباقيه و رسوبية تكوين افرومان (الترياسي)‎، شمال شرق العراق

Dissertant

al-Talibani, Muhammad Jamil Ali

Thesis advisor

Kyara, Ali Dawud

Comitee Members

al-Khafaji, Abd al-Sattar J.
Ismail, Sabah A.
al-Shaykhali, Sad Sami Jasim
Nasir, Midhat E.
al-Bayati, Fawzi Mardan

University

University of Baghdad

Faculty

College of Science

Department

Geology Department

University Country

Iraq

Degree

Ph.D.

Degree Date

2013

English Abstract

The Avroman Formation is exposed in the Iraqi Zagros suture zone along the Iraqi-Iranian border.

Four exposed section were studied with maximum thickness of 680m.

These sections are the Hanay Din, Nawe, Kani Seif and Dizly sections.

All sections are mainly composed of limestone interbeded with recrystallized dolomitic limestone and brecciated limestone.

The Nawe section may serve to proposal as type locality of the Avroman Formation in Iraq.

Three units can be recognized within the studied succession, each unit has a specific characteristic feature (U1, U2, & U3).

These units are separated by marker beds of recrystallized dolomitic limestone and brecciated limestone.

The Avroman carbonates consist of limestone with exception of two samples which are dolomitic limestone (8CN), while the second one is Brecciated limestone (38N).

Insoluble residue consists mainly of clay minerals (Smectite, mixed layer, Illite, and Kaolinite) and detrital minerals (Quartz and Foresterite).

Geochemical study shows that (CaO) is the main major oxide (34-56 wt%), and the Avroman carbonate rocks can be divided into three different groups according to its mineral composition.

Five main types of microfacies have been recognized, these include Mudstone, Mudstone-Wackestone, Wackestone, Wackestone-Packstone and Packstone microfacies.

The Avroman Formation was deposited on a shallow carbonate platform, most probably on a homoclinal ramp setting were gradual transition of shallow marine to deep marine conditions.

The Avroman succession can be divided in to a number of third order cycles, these cycles are mainly asymmetrical.

Main Subjects

Earth Sciences, Water and Environment

No. of Pages

100

Table of Contents

Table of contents.

Abstract.

Abstract in Arabic.

Chapter One : Introduction.

Chapter Two : Petrology.

Chapter Three : Geochemistry.

Chapter Four : Pale environments and sequence development.

Chapter Five : Conclusions and recommendations.

References.

American Psychological Association (APA)

al-Talibani, Muhammad Jamil Ali. (2013). Stratigraphy and sedimentology of the avroman formation (Triassic) northeastern Iraq. (Doctoral dissertations Theses and Dissertations Master). University of Baghdad, Iraq
https://search.emarefa.net/detail/BIM-609663

Modern Language Association (MLA)

al-Talibani, Muhammad Jamil Ali. Stratigraphy and sedimentology of the avroman formation (Triassic) northeastern Iraq. (Doctoral dissertations Theses and Dissertations Master). University of Baghdad. (2013).
https://search.emarefa.net/detail/BIM-609663

American Medical Association (AMA)

al-Talibani, Muhammad Jamil Ali. (2013). Stratigraphy and sedimentology of the avroman formation (Triassic) northeastern Iraq. (Doctoral dissertations Theses and Dissertations Master). University of Baghdad, Iraq
https://search.emarefa.net/detail/BIM-609663

Language

English

Data Type

Arab Theses

Record ID

BIM-609663