Volume 4 Issue 1

Published: 2025-06-25

Contents


Article
Geomorphology of Kand Structure North of Iraq Using Remote Sensing Data

Rayan G. Al-Banaa, Hekmat S. Al-Daghastani, Amer D. Nader,

Remotly sensed data were used in the study of the morphotectonic of the Kand Structure in north of Iraq .The present study showed that the landforms can be interpreted and analyzed depending on the...

DOI: 10.33899/earth.2004.37764

Pages: 58-73
Hydrologic System Observation and Rainwater Harvesting in SinjarRemote Sensing DataAlluvial Fans in the North of Jabel Using Remote

Taha H. AL-Salim Bashar M. AL-Shakergee, Hekmat S. AL-Daghastani,

The study area is located in the northwestern of republic of Iraq within the municipal boundaries of Nineveh Governorate within Sinjar Qadha. The landforms were analysed and classified using the...

DOI: 10.33899/earth.2004.37767

Pages: 15-28
Microfacies Analysis of Oligocene Formations in Butmah and Rafan Areas Northwest Iraq.

Nabil Y. Al-Banna,

Oligocene deposits in Butmah and Rafan areas northwestern Iraq were penetrated by three core holes (BW-CH1, BE-CH1 and RF-CH1). The depositional basin evolved through two stages, generating two...

DOI: 10.33899/earth.2004.37780

Pages: 8-21
Mineralogical Maturity, Weathering Index, Climate and Tectonic Setting of Injana Formation Based on Petrographic Constituents of Sandstones in Komal Syncline–North Iraq

Thamer A. Aghwan,

Petrographical study of Injana Formation showed that the sandstones are composed of quartz, feldspars, high proportion of rock fragments, other components and carbonate cement. The sandstones are...

DOI: 10.33899/earth.2004.37763

Pages: 47-57
Distribution and Evolutionary Trends of The Upper Tertiary OstracodeArabian Gulf.Cretaceous- Lower From Iraq and Arabian Gulf.

Nisreen M. Aziz,

The Ostracode biostratigraphic evidence and the evolutionary trend of Upper Cretaccous-Lower Tertiary Ostracodes are determinated by using the vertical and lateral distribution and the...

DOI: 10.33899/earth.2004.37796

Pages: 74-85
Determination of Fold Profiles and Fold Functions,

Nabeel K. Al -Azzawi,

Two mathematical approaches dealing with fold profiles and their clips of computer programs are adopted in this paper. The first is a mathematical method proposed for determining fold profiles...

DOI: 10.33899/earth.2004.37782

Pages: 22-35
The Use of Chemostratigraphy in Determining The Boundary Between Al-Fat`ha Fn. (Middle Miocene) and Injana Fn.

Hazim J. Al-Nuaimi, Abdul-Hadi Y. Al-Sayegh,

Chemostratigraphy is used to determine the boundary between the sandstones of Al Fat`ha Formation (Middle Miocene) and Injana Formation (Upper Miocene) at Ba`cheqah Mountain, the north east of...

DOI: 10.33899/earth.2004.37772

Pages: 1-14
Factor Analysis of Water Quality in Hit–Cubaisa Area, West of Iraq

Mohammed Faozy Omer Khattab,

This study involves the use of factor analysis technique to evaluate the chemical analysis results of (58) water samples taken from Hit-Cubaisa in the western part of Iraq. The samples were taken...

DOI: 10.33899/earth.2004.62055

Pages: 98-110
Biostratigraphy of Planktonic Foraminifera in Aaliji and Jaddala Formations From East Baghdad Well No.2 , Middle Iraq

Abdullah S. Al-Hadidi, Farouk S.Al-Omari,

Planktonic foraminifera are studied from Aaliji and Jaddala Formations in East Baghdad Well No.2 between the depth interval 1770-1900 m. Four biostratigraphic zones are recognized in these...

DOI: 10.33899/earth.2004.37777

Pages: 86-97
Landslides Along Makhul Range (Msa`hak Dome)

Varoujian K. Sissakian Safa Al-Deen Fouad Hala A. Salih,

Three large landslides have developed along the northern limb of Sa`hak dome, within Mkhool Range, which extends parallel to the Tigris River. The slided masses belong to the uppermost part of the...

DOI: 10.33899/earth.2004.37770

Pages: 1-7
Facies Analysis of The Ghar Formation at Selected Wells of South and Southeast Iraq

Ali Al-Jubory - Mohammad AL-Rubaii, Jamal S. Al-Ghrear,

Facies analysis of the Ghar Formation at selected wells of south and southeastern Iraq, promote the subdivision of the formation into two main facies. Sandy gravel and carbonates facies that...

DOI: 10.33899/earth.2004.37766

Pages: 29-46