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Geology of Algeria
The geology of Algeria is diverse; the country divides into three different tectono-stratigraphic domains. In the south and west is the West African Craton which consists of Precambrian granitic basement and surrounding Neoproterozoic mobile belts. Further south the Tuareg Shield comprises the Hoggar, Adrar des Iforas and Air sub-shields which have each been affected by tectono-thermal events touching much of the continent. In the north are the Alpine chain mountains with a succession of folded and over-thrusted strata.〔(Algeria Geology, The Extractive Industries Source Book )〕
==Economic geology==
The production of oil and gas are important to Algeria’s economy, being Africa’s main producer of the latter. Its reserves were estimated at 4.502 trillion m3 at the end of 2008. Productive fields are found in anticlines, faulted anticlines or domes; the reservoirs being in Cambro-Ordovician, Triassic, Devonian, and Carboniferous sandstones. Caprocks include Triassic evaporites and Carboniferous to Devonian shales. The major source rocks for the hydrocarbons were Silurian shales rich in organic material. In 2008, Algeria was the fourth largest oil producer in Africa accounting for about one sixth of the continent’s production. The country’s proven reserves of crude petroleum are out at 1.66 billion tonnes, or about 1 per cent of the global reserve.〔(Algeria, The Extractive Industries Source Book )〕
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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