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2 edition of geology of the dyke swarms of the Khor Sagesota area, Northern Red Sea Hills, Sudan. found in the catalog.

geology of the dyke swarms of the Khor Sagesota area, Northern Red Sea Hills, Sudan.

Salah Eldin Mohmed Nour

geology of the dyke swarms of the Khor Sagesota area, Northern Red Sea Hills, Sudan.

by Salah Eldin Mohmed Nour

  • 193 Want to read
  • 30 Currently reading

Published by Portsmouth Polytechnic, Dept. of Geology in Portsmouth .
Written in English


Edition Notes

Thesis (M.Phil.) - Portsmouth Polytechnic, 1983.

ID Numbers
Open LibraryOL13835432M

The Ministry of Mining Strategic Plan has been prepared within the framework of South Sudan Vision whose aspiration is “Towards Freedom, Equality, Justice, Peace and Prosperity for all” and the Guiding Principles and Values, which include Democracy, Rule of Law; Socio-Economic Development; and International Relations. The Red Sea (Arabic: البحر الأحمر Al Baḥr al aḥmar ‎, Hebrew: Yam Soof ים סוף) is a seawater inlet of the Indian Ocean, lying between Africa and connection to the ocean is in the south through the Bab el Mandeb strait and the Gulf of the north lie the Sinai Peninsula, the Gulf of Aqaba, and the Gulf of Suez (leading to the Suez Canal).Coordinates: 22°N 38°E / 22°N 38°ECoordinates: .

Marks describes and defines the Khormusan industry. The industry was first recognized with the excavation of sites and ANW-3 in Only five sites represent the Khormusan industry. (Marks dates the industry from approximat to 16, B.P., while Fred Wendorf, who wrote the culture summary for Middle Paleolithic Egypt in the Encyclopedia of Prehistory dates site from Cited by: Regional Geology and Ground water Hydrology of the Sahil Susah Area, Tunisia. [L. C. & H. E. Thomas. Dutcher] on *FREE* shipping on qualifying offers.

Other articles where Kangamiut dike swarm is discussed: Precambrian: Basic dikes: billion-year-old Kangamiut swarm in western Greenland is only about km ( miles) long but is one of the world’s densest continental dike swarms. Many of the major dike swarms were intruded on the continental margins of Proterozoic oceans in a manner similar to the dikes. Sudan is located in northeastern is bordered by Egypt to the north, the Red Sea to the northeast, Eritrea and Ethiopia to the east, South Sudan to the south, the Central African Republic to the southwest, Chad to the west and Libya to the northwest. Sudan is the third largest country in Africa, after Algeria and East had been the largest country on the continent until the.


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Geology of the dyke swarms of the Khor Sagesota area, Northern Red Sea Hills, Sudan by Salah Eldin Mohmed Nour Download PDF EPUB FB2

Perhaps the most comprehensive study of the dykes in the Red Sea Hills of Sudan so far is an unpublished work by Abu Fatima (). He divided the dykes into two main groups: older dykes and younger by: Khor Kharfot is part of a coastal estuarine wetland system located in the western part of the Dhofar Governorate preserving a pristine ecosystem supporting a distinct vegetation and animal habitat.

A sand barrier along the khor (local term for wetlands) mouth controls the mixing of fresh and marine water in the enclosed lagoon. part of the area.

Hoorn and Cremaschi [5] is the only work available on the geology of Dhofar khors, including Khor Al-Balid and Khor Rawri near Salalah. The present study is the first of its kind to map the Holocene deposits of Khor Kharfot in the Jabal Qamar area.

The khor was mapped with the help of a topographic base map and Google by: 1. Here we present results of a study of more than Northern Red Sea Hills, mostly mafic and fresh, dykes from the Haya area, located at the west margin of the Red Sea in the Red Sea Hills of Sudan.

The dykes belong to. The regional dyke swarms of the Red Sea Hills have been known for some time (Whiteman,Vail and Hughes,AbuFatima, ), but no recent systematic studies have been published on their structural and geometrical aspects or their influence on groundwater Northern Red Sea Hills The effects of dykes and faults on groundwater flow in an arid land: The Red Sea Hills, Sudan Article in Journal of Hydrology (1) April with Reads How we measure 'reads'.

in Sudan and include the Ennedi, Erdis, and Tibesti Mountains as well as the Hamada desert area of Fezzan in Libya (Himida ). The eastern side of this desert is limited to the Nile Valley.

The southern margins are distinguished by the Darfur and Kordofan mountainous areas in Sudan, while the desert extends to the north until it reaches the. Sudan has been chronically plagued by civil war and, inwas sanctioned by the United Nations for sponsoring terrorism.

A civil war in Yemen ended in Eritrea and Ethiopia have had recent conflicts. Geologic Setting The Red Sea Basin Province originated as an Oligocene continental rift impacted by left-lateral wrenching.

Outlines of the geology of Sudan Sudan geological study was focused on the surface geology mainly for surface mapping and limited shallow mining activities. With the recent discovery of commercial hydrocarbon, extensive subsurface data has been acquired both offshore and onshore.

Other articles where Dike swarm is discussed: South America: The Trans-Amazonian cycle: platform deposits; and large extensional dike swarms (groups of tabular intrusions of igneous rock into sedimentary strata). The orogenic belts represent old mountain chains that had been formed either along the margins of the continent as geosynclines (downwarps of Earth’s crust) and then uplifted.

representatives from South Sudan are for the first time shedding light on the country’s artisanal and small-scale mining sector. The picture that emerges is a remarkable one: artisanal gold mining in South Sudan ‘employs’ more t people and might indirectly benefit almost half a million people.

Geology and Mineral Investment Opportunities in South Sudan Hosted by Dr Andu Ezbon Adde, Under Secretary Mining, South Sudan Mining On Top: Africa - London Su Slideshare uses cookies to improve functionality and performance, and to provide you with relevant advertising.

The Red Sea Rift has been an object of comprehensive studies by several generations of geologists and geophysicists. Many publications and open-file reports provide insights into the geological history of this rift. Paleogene and Cretaceous rocks, which are considered to be prerift, are locally exposed at the margins of the Red Sea Rift.

At the same time, some evidence indicates that at least Cited by: 6. The wealth of petroleum has made the Middle East one of the most actively explored regions of the world.

The volume of geological, geophysical and geochemical data collected by the petroleum industry in recent decades is enormous.

The Middle East may be a unique region in the world where the volume of subsurface data and information exceeds that based on surface outcrop.3/5(3). once erupted there, and in Kordofan there are many rocky hills which are collectively called the Nuba Mountains.

In the north-east of the Sudan occurs the long range of the Red Sea Hills which extend into Egypt. Elsewhere, the Sudan plain is only occasionally broken by isolated "jebels" which rise sharply from the flat ground.

Sudan and South Sudan are two of nearly countries illustrated on our Blue Ocean Laminated Map of the World. This map shows a combination of political and physical features. It includes country boundaries, major cities, major mountains in shaded relief, ocean depth in blue color gradient, along with many other features.

The area of Gebeit Mine in the northern Red Sea Hills, Sudan, is built up of voluminous volcanic rocks and minor volcaniclastic and clastic sequences. According to their chemical and modal compositions the Gebeit volcanics can be devided into four groups: (a) cpx-physic basalts with clinopyroxene and plagioclase as the dominant phenocrysts and minor opaques; (b) hbl-physic Cited by: • With such big area and diversified geology which merges across the boundaries between nine countries Sudan has a huge mineral potential yet to be evaluated and developed.

• The Ministry of Minerals, through the Geological Researches Authority of the Sudan (GRAS), the State Geological File Size: 2MB. Science and Technology, Khartoum P. Box: 72, Sudan, 2-Department of Geology and mind, College of Natural Resources and Environmental Studies – University of Juba – Sudan.

ABSTRACT Muglad Basin is recognized to be a major part of Sudanese interior rift basins. It trends northwest-southeast covering an area of over km long and. Title: Groundwater balance in the Khor Arbaat basin, Red Sea State, eastern Sudan: Authors: Elsheikh, Abdalla E.

M.; Zeielabdein, Khalid A. Elsayed; Babikir, Ibrahim A. Affiliation: AA(School of applied Earth Science-Faculty of Science and Technology Al Neelain University - Sudan, Khartoum, Sudan), AB(School of applied Earth Science-Faculty of Science and Technology Al Neelain University. Erkowit, a Neolithic Site in the Red Sea Hills (Sudan): interim report on the pottery by Ghanim Wahida and Abdelrahim M.

Khabir — Sudan & Nubia, No 7, published by The Sudan Archaeological. Purchase Sedimentary Basins and Petroleum Geology of the Middle East - 1st Edition. Print Book & E-Book.

ISBNBook Edition: 1. History of South Sudan. The Nilotic peoples—the Dinka, Nuer, Shilluk and others—first entered South Sudan sometime before the 10th century. During the period from the 15th to the 19th centuries, tribal migrations, largely from the area of Bahr el Ghazal, brought these peoples to their modern locations.