Exploratory activities carried out by oil companies in the latter half of the past
century proved the existence of voluminous reserve of oil and gas in the
southwestern area of Iraq. In view of this, it seemed more than prudent to add a new
knowledge to that currently existing about the subsurface lithostratigraphy of this
area. As a first step in fulfilling this mission, this paper will attempt to do so by
covering the time interval from the Upper Cretaceous to the Neogene. In turn, this
effort had entailed both the description of about 4707 metres of fully recovered
cores, plus the subjection of more than 4000 samples to existing petrologic analyses.
Findings worth mentioning does include the observation that with the exception of
the Paleogene sequence, the Upper Cretaceous and Neogene sequences are no
different from those found in other parts of southern Iraq. For instance, the Upper
Cretaceous sequence is found to be consisted of the common Hartha, Qurna, and
Tayarat Formations. The same could be said about the Neogene sequence which is
found to be again made of the common Ghar, Euphrates, Fatha, and Zahra
Formations. In contrast, the Paleocene – Lower Eocene sequence lithology is found
a bit different from those commonly encountered in other parts of southern Iraq.
This difference emanates from the intense sulphidzation as manifested in the
common occurrence of anhydrite, gypsum, and vanished evaporite being observed
through the lower Paleogene sediments of south west, Iraq. Because this
phenomena exhibits strong vertical as well as lateral variation, this sequence is
divided into an intensely evaporitic portion, which is introduced in this article under
the name of the Jerishan Group (Paleocene - Lower Eocene), inclusive of Umm Er
Radhuma, Rus, Jil/Rus, and Jil Formations. The latter formation is recently
introduced stratigraphic rock unit representing the non-evaporitic equivalent for the
Rus Formation. The less evaporitic portion (the Dammam Formation) of the
Paleogene was found to be the same as the ones found in other parts of the south
Iraq, Kuwait and Saudi Arabia.
The Aqra - Bekhme, Shiranish, Tanjero and Kolosh formations outcrop in the High Folded Zone, Northern Iraq in Erbil and Sulaymaniyah governorates. The formations have been studied at two selected geological sections (Bekhme Gorge and Zarda Bee). In this study, these formations are investigated based on both benthic and planktonic foraminifera. Depending on foraminifer’s investigation, three biozones have been recognized; two biozones are identified in the benthic foraminifera and the third one is identified in the planktonic foraminifera as follow:
- Siderolites calcitropodes - Orbitoides apiculatus - Omphalocyclus macroporus Assemblage zone.
- Loftusia morgani range zone.
- Aba
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The Fort Munro Formation is well exposed along DG Khan-Fort Munro road, a type locality. The section was measured and sampled for the biostratigraphy, where it has a conformable lower contact with Mughalkot Formation and is underlain by the Pab Sandstone. The total observed thickness was 105 meters, and 26 samples were collected from top to the bottom at random intervals. Fifty thin sections were studied carefully, and five species of large benthic foraminifera, including Orbitoidestissoti, Orbitoidesapiculata, Orbitoides media, Orbitoideshottingeri, and Omphalocyclusmacroporus were identified along with miliolids. Gastropods, Bivalves and Echinoderms were also observed. Based on identified microfossils, the de
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Graceful labeling of a graph with q edges is assigned the labels for its vertices by some integers from the set such that no two vertices received the same label, where each edge is assigned the absolute value of the difference between the labels of its end vertices and the resulting edge labeling running from 1 to inclusive. An edge labeling of a graph G is called vertex anntimagic, if all vertex weights are pairwise distinct, where the vertex weight of a vertex under an edge labeling is the sum of the label of all edges incident with that vertex. In this paper, we address the problem of finding graceful antimagic labelin for split of the star graph , graph, graph, jellyfish graph , Dragon graph , ki
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Ten samples were collected from Injana and Mukdadiya Formations, representing 5 samples of fine grain sandstone (F) and 5 samples of very fine grain sandstone (VF). The heavy metals study showed that the opaque mineral recorded the highest percentage in comparison with other heavy metals. While, transparent minerals, including unstable minerals (Amphibole including Hornblend and Glaucophane) and (pyroxene including Orthopyroxene and Clinopyroxene), Metastable minerals including (Epidote, staurolite, Garnet, Kyanite) indicated metamorphic source, Ultrastable minerals (Zircon, Rutile, Tourmaline), Mica group (chlorite, biotite and muscovite). These accumulations indicate that the heavy minerals are derived from mafic igneous and metamorphi
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This study deals with the seismic reflection interpretation of Cretaceous Formations in Tuba oil field, southern Iraq, including structural and stratigraphic techniques. The study achieved by using Geofram , Geolog and Petrel software. The interpretation process, of 2-D seismic data and well logs have been used. Based on well logs and synthetic traces two horizons were identified and picked which are the tops of Mishrif and Zubair Formations. These horizons were followed over all the area in order to obtain their structural setting. Structural interpretation indicates that the Tuba oil field is an anticline structure as well as the presence of normal fault near Mishrif Formation trending NE-SW. Information from the wells appeared Mishrif
... Show MoreThe study deals with 3D seismic reflection in the central Iraq within Merjan oil field which is located approximately (130 km) to the southwest Baghdad and south of Razaza. The 3D seismic survey was interpreted; the results showed that the oil is found within Hartha Formation as stratigraphic traps and with the absence of structural traps. The major normal faults picked are trending N-S direction. There are also minor faults observed using the instantaneous phase and frequency sections, they proved the presence of the faults and showed that the ending of the Safawi reflector toward the north and northeast to the south and southeast and near the western border of fault because of the facies change in the area. The reflector shows a struct
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