YEMEN - Maarib/Jawf BackgroundDespite the long neglect of Yemen's interior by foreign companies, the geology of that area remained the subject of interest, particularly in the north-east of Maarib. As a result, the Sanaa government in 1979 sponsored an aero- magnetic survey. The results of that survey in 1980 caught the attention of Moujib Al Malazi, a Syrian exploration consultant to Ray Hunt's Hunt Oil Co. of Dallas. He studied data showing a narrow but deep graben with a thicker sedimentary basin The term sedimentary basin is used to refer to any geographical feature exhibiting subsidence and consequent infilling by sedimentation. As the sediments are buried, they are subjected to increasing pressure and begin the process of lithification. than originally thought. He shared his assessment with Dr. Ian Maycock, exploration manager of Hunt Oil's London office, and the two concurred that Pre-Cambrian rock formed the basis for the entire area, later known as the Maarib/Jawf Basin (also known as the Sabatayn Basin). There was a sharp boundary in the north-west with a Jurassic formation, which in Saudi Arabia Saudi Arabia (sä `dē ərā`bēə, sou`–, sô–), officially Kingdom of Saudi Arabia, kingdom (2005 est. pop. has yielded prolific oil reservoirs An oil reservoir, petroleum system or petroleum reservoir is often thought of as being an underground "lake" of oil, but it is actually composed of hydrocarbons contained in porous rock formations. .
The theory was that the north-west/south-east trending graben had
started to rift in Jurassic times and accumulated a good thickness of
sediment.
In December 1980 Maycock took the data and Malazi's assessment to Ray Hunt in Dallas. Within days Hunt sent a team to Yemen for a further scouting of that area and started negotiations with the Sanaa government. (Now Hunt is producing 140,000 b/d of light/sweet crude oil from that area - down from 169,000 b/d in mid-1996 and almost 200,000 b/d in 1992. Saudi Arabia in 1992/93 included the Maarib/Jawf region among areas it claimed to be part of its territory). Addressing a London Geological Society conference in 1990, Maycock explained that the government's 1980 survey had indicated the possibility of a 30,000 sq km sedimentary basin and a fill of 3,500 metres. Subsequent successes achieved by Hunt Exploration Co., he said, were a fine example of rich rewards gained by perseverance and an imaginative exploration in frontier areas. The Maarib/Jawf area was mostly covered in sand but included a diapric salt anticline anticline: see fold. with some associated bituminous shales an argillaceous shale impregnated with bitumen, often accompanying coal. See under Bituminous. See also: Bituminous Shale . Close to the basin centre, there was also a basement outcrop. Field work along the margins revealed a Mesozoic sequence 750 metres thick, including important Upper Jurassic sands rich in oil. On evidence of likely source rocks, the prime targets for Hunt were: possible reservoirs, evaporites to provide structuration The theory of structuration, proposed by Anthony Giddens (1984) in The Constitution of Society, (mentioned also in Central Problems of Social Theory, 1979) is an attempt to reconcile theoretical dichotomies of social systems such as agency/structure, and seals, amenable government regulations and, most importantly Adv. 1. most importantly - above and beyond all other consideration; "above all, you must be independent" above all, most especially , a potentially large oil basin. Subsequent studies concluded that the then shared North-South Yemen border zone nearby, called Wadi Al Ain This article is about the city in the United Arab Emirates. For the city in Lebanon, see El Ain. Al Ain (Arabic: العين (later to be known as Jannah block), also contained related strata. The Amal and Iyad oilfields in Shabwa of the southern sector, only about 55 km east of Maarib's Alif field, were found to be of a similar Upper Jurassic reservoir. Later it was proven that they all had the same basin, which aroused the interest of many companies. |
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`dē ərā`bēə, sou`–, sô–)
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