Partnering with the Republic of Sudan to transform natural resources into mutual prosperity. We find, develop, and own the best assets to deliver sustainable returns.
Sudan is among the largest countries in Africa and characterized with diversified geological units and structure that host great and variable numbers of minerals wealth.
The area between the Nile and the Red sea, South Kordofan, and South Darfur.
Red Sea Hills.
Iron at Red Sea Hills. Chromite at Ingessana, Nuba Mountains, Red Sea Hill, and Qala En Nahal.
Red Sea Hills, Bayuda Desert, Ariab Region, and Hofrat En Nahas.
Abu Samar area, Tagoteb, Um Takatik at NE-Nuba Mountains. Lead at Kutum, North Darfur.
Bayuda, Red Sea Hills, coastal plane, and North Port Sudan (Gypsum).
Red Sea Coastal (contains magnetite, ilmenite, rutile, and zircon).
Agricultural (Phosphate), Kaoline, Talc, Magnesite, Feldspars, Fluorspar, Barite, White Gold.
Opal Mining Co. Ltd signed concession agreement for the exploration, development and exploitation of gold and association metals.
Sahara Desert
~300 sq. km
Lat 21°20'25" – 21°12'37"
Lon 31°42'0.00" – 31°30'0.00"
Khartoum to Abu Hamad (470km) via National Hwy.
Abu Hamad to Wadi Halfa (Station 6) (165km) via Railway.
Station 6 to Concession (55km) via Unpaved Road (4x4).
Total Distance: ~690km.
The concession area domain is situated in the western margin of the Nubian Desert, whereby more than 50% of the surface area is covered by sand dunes. The thickness of the sandy sheets varies from place to place, but in most localities reaches a few meters above the surrounding. Most of the ridges and basement inselbergs are scattered in this area. Low-lying basement outcrops are exposed as peneplains. The topography of the south of the Block is covered by low-lying Nubian Sandstones.
The concession is part of the Sahara Desert and thus the prevailing climate is dry with less than 50mm per year rainfall in the period from July to September. The winter season is from November to February in which the daily temperature may drop to 15°C. Otherwise, the climate is very dry and hot, the daily mean temperature ranges from 35°C to 42°C.
The Precambrian geology in NE Africa comprises two distinct crustal domains; The Nile Craton and the Arabian-Nubian Shield (Stern, 1994; Kröner, et al. 1987a; Vail, 1983; 1988; Rocci, 1965).
The area covered by Bayuda Desert is relatively well studied compared to other areas in northern Sudan (Vail, 1971; Barth and Meinhold, 1979; Dawoud, 1980; Ries, et al, 1985). Wadi Halfa and Bayuda Terrains (Schandelmeier, et al, 1994) represent the reworked eastern foreland of the Nile Craton, while Gabgaba Terrain (Abdelrahman, 1993) represented the westernmost part of the Arabian-Nubian Shield (ANS). Wadi Halfa area poorly understood due to the limited studies conducted in the area (Stern, et al, 1994; Griffiths, et al, 1987).
According to previous studies in north and northeast Sudan, the litho-stratigraphic units of the Wadi Halfa-Bayuda-Gabgaba area are (Denkler, et al, 1994; Abdelrahman, 1993; Vail, 1988; Barth and Meinhold, 1979):
Ministry of Minerals, Khartoum.
Official signing ceremony securing exploration rights.
Over 3 decades experience in Investment, Mining and Financial Management across Africa and the UAE. Extensive strategic links to China, the Middle East, and Asia forming the foundation of Opal Mining.
Executive with extensive experience across the UN, USA, Malaysia, Libya, UAE, and South Africa. Expertise in corporate strategy across diverse international disciplines and cultures.
Prominent banker and strategist to African governments and multi-billion dollar corporations. Managed >US$600 million of donor flows at Citibank across multiple African nations.
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20+ years driving global IT operations. Technical architect specializing in secure remote infrastructure, ensuring robust and compliant data networks for continuous corporate operations.
Al Sayid Ali Al Merghani Street
Khartoum North (Bahri), Sudan.
chakik@consultant.com
00249991959595
00905449601119