The Jeed Formation (Upper Maastrichtian to Lower Danian) in the Western Desert of Iraq is a new proposed mixed lithostratigraphic succession containing various rock types, including phosphatic, siliceous, calcareous, siliciclastic, and other mineralogical contents (carbonate flouraptite, quartz, calcite, dolomite, opal-CT, smectite, palygorskite, sepiolite, kaolinite, and locally zeolite). The current study presents a review compliant with ICS standards and a revised lithostratigraphic framework for the Jeed Formation, based on a synthesis of historical usage, stratigraphic evolution, and previous miscorrelations, along with contributions from new data from integrated lithological, mineralogical, and microfacies datasets. The formation has been formally redefined and recognized as the correct stratigraphic unit, thus replacing the earlier misapplied Upper Campanian-Lower Maastrichtian Digma Formation in Western Iraq. The Jeed Formation consists of two members: the Upper Maastrichtian Safra Member and the Lower Danian Trafawi Member, each subdivided into two beds: lower and upper. The upper Maastrichtian member shares the same depositional phase as the lower Danian member, with a symmetrical lithological architecture and comparable depositional basins, indicating a series of identical lithofacies controlled by regional and continental factors rather than local ones. The Cretaceous-Paleogene (K/Pg) transition is marked by a geologically significant unconformity that extends across the entire region and serves as a marker for the Safra /Trafawi member boundary. Regional correlation between the Muwaqqar Chalk Marl Formation of Jordan, the Jalamid Formation of northern Saudi Arabia, and the Dakhla Formation of Egypt highlights the role of the Jeed Formation within a continuous Maastrichtian–Danian phosphogenic belt along the southern margin of the Tethys Ocean.
This paper deals the prediction of the process of random spatial data of two properties, the first is called Primary variables and the second is called secondary variables , the method that were used in the prediction process for this type of data is technique Co-kriging , the method is usually used when the number of primary variables meant to predict for one of its elements is measured in a particular location a few (because of the cost or difficulty of obtaining them) compare with secondary variable which is the number of elements are available and highly correlated with primary variables, as was the&nbs
... Show MoreThe measurements of major and trace elements in different brands of milk powder selected from the Iraqis market via the X-ray fluorescence (XRF) Technique have been studied in the present work. The result of the measurements reveals the high concentrations of sodium, phosphorus, sulfur, chlorine, potassium, calcium and magnesium. Furthermore, low concentrations of aluminum, silicon, iron, bromine, molybdenum, iodine, barium, titanium, manganese, cobalt, chrome, nickel, copper, zinc and lead were detected. Neutron activation analysis (NAA) and Kjeldahl technique were also employed to determine the concentrations of nitrogen. It was found that the nitrogen concentration was in the range of (1.96 - 3.23) % which is within the permissible li
... Show MoreIn petroleum reservoir engineering, history matching refers to the calibration process in which a reservoir simulation model is validated through matching simulation outputs with the measurement of observed data. A traditional history matching technique is performed manually by engineering in which the most uncertain observed parameters are changed until a satisfactory match is obtained between the generated model and historical information. This study focuses on step by step and trial and error history matching of the Mishrif reservoir to constrain the appropriate simulated model. Up to 1 January 2021, Buzurgan Oilfield, which has eighty-five producers and sixteen injectors and has been under production for 45 years when it started
... Show MoreA cut-off low is a closed low with a low value of geopotential height at the upper atmospheric levels that has been fully detached (cut-off) from the westerly flow and move independently. A cut-off low causes extreme rainfall events in the mid-latitudes regions. The main aim of this paper is to investigate the cut-off low at 500 hPa over Iraq from a synoptic point of view and the behavior of geopotential height at 500 hPa. To examine the association of the cut-off low at 500 hPa with rainfall events across Iraq, two case studies of heavy rainfall events from different times were conducted. The results showed that the cut-off low at 500 hPa with a low value of geopotential height will strengthen the low-pressure system at the surface, lea
... Show MoreIn light of crises, the need for efficient and flexible public administrations to make quick and decisive decisions, also institutions capable of directing the internal elements and components of them and adapting them to the requirements of rapid change due to crises and disasters, which led to scarce resources becoming scarcer and economic, political and social problems becomes more prominent. For the majority of developing countries, including Iraq, the increasing need for the importance of moving towards enhancing the efficiency of the performance of public institutions while trying to predict their future, can only be achieved. Through solid mechanisms and principles of governance that enhance the ability of institutions and make them
... Show MoreThe Iraqi culture faced a set of challenges that can be diagnosed with the most prominent features as follows:
- The dominance of authoritarian political systems which entails authoritarian regimes with the absence of contemporary political concepts of human rights.
- The prevalence of non- informed cultural systems which have the shortage of capabilities that enable them to activate cultural elements in positive references, historical, or seclusion on itself and not be able to interact with the current active cultures.
- Stagnant economic conditions have not had a decent life for individuals, or a certain level of well-being, as well as poor services and others.
- Social life controlled by the prevai