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  1. 1. OIL AND GAS PROSPECT IN THE YEMENI SECTOR OF THE RUB AL-KHALI BASINWang Xikui* and Nedham Mohammed Darsi**(Changchun University of Science and Technology, 130026, China)ABSTRACTThis is the first paper, which discusses the Oil and Gas Prospects in the YemeniSector of the Rub al Khali Basin on the basis of a new look to the area. This newlook to the area depends:1. The geological research history work in the area,2. The neotectonic movement,3. The new crust movement,4. A collection of satellite images, which had been taken of the Republic of Yemenduring the period from 1994 to 1997 with hundreds of airophotos and satellite images,taken to different part of the Peoples Republic of China. (As an exemplars to find acase study to the Yemeni Sector of the Rub al Khali Basin). And this led us tointroduce a new idea for a new project, which we hope is going to help futurepetroleum exploration activities and attract foreign exploration investment to work inthe Yemeni sector of the Rub al Khali Basin.1 INTRODUCTION:It is known that one of the worlds largest exploration successes of the 1980s was thediscovery, by Canadian Occidental and partners, of constellation of oil pools in theMasila region of Yemen. The presence of several hundred million barrels ofrecoverable oil has been proved by drilling within reservoirs ranging in age fromJurassic to Cretaceous, with most reserves in Lower Cretaceous sandstone of theQishn Formation. The discovery of commercial oil and gas in several interiorMesozoic rift basins of Yemen in the late of 1980s and in the early 1990s after theYemeni unification, spurred many oil companies to enter the exploration race andcarry out detailed seismic surveys. This led to intensive explorations drilling in manyareas. The Yemeni sector of the Rub al Khali Basin, the main subject of this paper, isone of those areas, which found some care in the past and attracts many oil companiesin the present time.Note (1):(a) Al-Ghawar oil field one of the worlds largest oil fields has been found in the Rubal Khali Basin.(b) Oil, which is exploited in thats area is of excellent quality.(c) Oil Companies, which drilled exploration wells in the Yemeni sector of Rub alKhali basin (in Qinab, Hathout and Shahr area), had penetrated Paleozoic clasticreservoirs with core porosity ranging between 5% and 25%, 120 md to 3200 mdpermeability and age from Middle Cambrian to Early Permian.(d) The Qusayba (lower Silurian) shales, which is the principal source rock forPaleozoic discoveries in Saudi Arabia is present in the above mentioned areas.
  2. 2. (e) Much of the southern flank of the basin lies within northeastern Yemen, with theregional Paleozoic Hadramawt Arch forming the southern basin margin onto whichall Paleozoic and Early Mesozoic sedimentary sequences pinch out.(f) Northward into the basin, the flank slopes gently but in a step-like manner and thesedimentary column thickness increases from about 2 km near the crest of theHadramawt Arch to over 4 km by the Yemeni-Saudi border.2. PERVIOUS ACTIVITIES:According to Nedham Mohammed Darsi** division of the geological researchhistory work in the Republic of Yemen can be classified to four stages (SeeYemen Times Newspaper. Issue 2-January 10th through January 16 2000, Vol.IX, Culture Page, Issue 10 - March 6 through March 12 2000, Vol. X, CulturePage and Issue 15 - April 10 through April 16 2000, Vol. X, Culture Page). It isso clear now, that:2.1 On the First Stage (The First Systematic Geological Observation Stage orCarters Stage), 1852-1901:No kind of geological studies had been detected in the area.2.2 On the Second Stage or the Hinterland Studies Stage, (1902-1946) and theThird Stage (The First Systematic more detailed Stratigraphic and GeologicalStudies Stage or Beydoun, Z.R.s Stage, (1947-1967):Geological field investigation, supplemented by photogeologic and ground mappingcovering the entire territory, were carried out by the Petroleum Concessions Ltd, oneof the Iraq Petroleum Company associated companies (IPC and Associatedcompanies) between 1937 and 1960.2.3 On The Third Stage (The First Systematic more detailed Stratigraphic andGeological Studies Stage or Beydoun, Z.R.s Stage), 1947-1967:Bunker, D.G. wrote about the southwest Borderlands of Rub al Khali, in 1953. From1961 to early 1967, Pan American International Oil Company through a subsidiary,Pan American Hadhramawt Oil Company (PAHOC) drilled four wells (Hoowarin,Tarfayt and Core Hole 88 reached Precambrian basement and the forth wasabandoned in the Cretaceous sediments).2.4 The Fourth Stage or The Yemeni Geologists Stage (1968 Ð until Today):2.4.1. It is known that, the Petroleum and Minerals Board (the PMB) was established,in 1970 in former South Yemen. During the period from 1970 to 1973, the joint offormer South Yemen-Algerian Petroleum Company (SYAPCO) drilled Taur-1 in1974 and Taur-2 was commenced. In 1974, a group of experts from Cuba assumed thedrilling operation from SYAPCO and with former PMB completed Taur-2, Taur-3and drilled Thamud-1 and Hathout-1. In September 1976, the functions of the PMBwere broadened and the Petroleum Exploration Board (the PED) was created (ThePetroleum Exploration and Production Board, Aden Branch Ð As known now), leddifferent activities on studying the geology of this area. As a result of their work onthe Yemeni sector of Rub al Khali basin, wells as Taur-2, Taur-3 and Hathout-1 wasdrilled. A group of the P.E.D.s Engineers, Technician and workers, work hard on thisarea, and their work is highly appreciated. On Mar. 27 1979, B. Kuzin andMohammed Baabad made a Stratigraphic Correlation, for wells drilled in that area
  3. 3. correlative with wells located in the adjacent area at that time.Note (2): The Petroleum Exploration and Production Board (P.E.P.B.) Ð isresponsible for all petroleum exploration and related activities and is interested withthe exploration for oil and gas in the Republic of Yemen on its own, or in associationwith foreign companies through production sharing agreements. The P.E.P.B. has aprofessional staff and other administrative personnel.2.4.2. Between 1975 and 1979, as a part of its assistance program, TechnoExport, theformer Soviet Technical Assistance Organization, had recorded aeromagnetic surveyscovering most of former South Yemen and also a gravity survey had been conductedover specific areas of interest. CDP reflection and refraction seismic had beenconcentrated in the Yemeni sector of Rub al Khali basin and as a result of their workin the area, wells as Hathout-2 Shahr-1 were drilled in 1981-82.Note (3): The field investigation had been augmented from time to time byCzechoslovakian and German technical personnel.2.4.3. In the Yemeni sector of the Rub Al-Khali basin, first Bahad flower structurewas detected from the seismic interpretation and then later Qinab flower structure haddetected from the seismic interpretation by Elf Acquitaine Petroleum B.V, during thefirst phase of exploration in their ex-block 11, in 1989.3. THE RUB AL-KHALI SAND DESERT:The Rub al Khali sand desert or the Empty Quarter (as also known) is a huge regionof sand covering about c.225, 000-sq. mi. (582,750 sq. km). It is one of the largestsand deserts in the world and the great desert of the Arabian Peninsula. Thdesertoccupies much of the southern interior of the peninsula, from the highlands of theNejd (to the north) to the plateaus of Hadhramawt (to the south); it slopes from analtitude of 3,300-ft (1,006 m) in the west to near sea level in the east. The sand dunesin the Rub al Khali sand desert rise to over 660 ft (200 m) in the southwest and mainlydistributed in parallel to sub parallel ridges (called uruq), separated by narrow flatstretches of gravel, gypsum, or silt (shuquq). The trend of the southern border of thedesert is east-northeast, which is also roughly the trend of the dune ridges. Slip facesof the dunes are generally south, but some north-facing slip faces have been observed.Some migration of dunes takes place; however, the migration seems to be up byseasonal wind directions, so that migration in any specific direction is difficult todetect; there are salt marshes and pans in the southeast. Rub al Khali is connected tothe Nafud desert in the north by the Dahna, a narrow corridor, 800 mi. (1,287 km)long. The desert comprises more than 25% of Saudi Arabia. It is extremely dry andvirtually uninhabited. Only the southernmost fringe of which reaches into theRepublic of Yemen. A much smaller area is the Ramlat Sabatayn sand desert. Itstretches eastward from the foothills in the north part of the Republic of Yemen and inBayhan province, where it is some 100 kilometers wide, into the Hadhramawtdrainage basin, occupying roughly the western extension of the Wadi Hadhramautstructural trough. The dunes lose both height and lateral extent eastward, until theydie out as low isolated patches of sand some five kilometers in width near Shibam inWadi Hadhramaut. The Ramlat Sabatayn area is again one of dune ridges which,however, are less regular than those of the Rub al Khali with a trend roughly east-northeast in the west, are some 50 meters in the height, and are eastward and become
  4. 4. irregular toward the east. Migration of the sand is largely offset by seasonal changesin the prevailing winds and by thermal disturbances.4. THE YEMENI SECTOR OF THE RUB AL-KHALI BASIN:Several depressions are superimposed on the Arabian Shelf and at one time foranother have received thick deposits relative to adjacent parts of the platforms. Suchbasinal sags have formed in the northeastern Rub al Khali, northern Persian Gulf,Dibdibah, and Sirhan Turayf areas. Seismograph and structural drill work in the Rubal Khali Basin have outlined an elongate basin. Width of the basin is relativelyuniform throughout its length, eraging about 300 km. It is known that the Yemenisector of the Rub Al-Khali basin forms the southern flank of this huge structuraldownwarp, which originated in the early Paleozoic as intracratonic sag later in thePaleozoic. This feature is bounded on the north by the sand dunes of the Rub al Khaliand on the south by theRamlat Sabatayn sand desert. Much of the southern flank of the basin lies withinnortheastern Yemen, with the regional Paleozoic Hadramawt Arch forming thesouthern basin margin onto which all Paleozoic and Early Mesozoic sedimentarysequences pinch out. Northward into the basin, the flank slopes gently but in a step-like manner and the sedimentary column thickness increases from abut 2 km near thecrest of the Hadramawt Arch to over 4 km by the Yemeni-Saudi border.5. SATELLITE IMAGES INTERPRETATIONAccording to our study on a collection of satellite images, which had been takento the Republic of Yemen during the period from 1994 to 1997 and hundreds ofairophotos and satellite images, which had been taken to different part of thePeoples Republic of China. We concentrated our attention onto the followingmore important satellite images, due to:5.1. Those satellite images were related to the Yemeni sector of the Rub Al-Khalibasin.5.2. The very clear images of different faults types shown on the surface, whichwe classified them according to their directions and trend, to:First type: Faults with a NEÐSW directions (very clear on the satellite images).Second type: Faults with EÐW and ENE-WSW directions (clear to very clear on thesatellite images).Third type: Faults with an NÐS and NNE-SSW directions (clear to very clear on thesatellite images)Forth type: Faults with a NWÐSE directions (clear to a little clear on the satelliteimages).
  5. 5. 5.3. According to the character of the Satellite images, we found a black materialfilling these faults on the surface, which looks like natural asphalt (?). Here wewant to drew People, who are interested in this field on the following fact:The same example was found in Kelamayi oil field, a famous oil field in theNorthwest of the Peoples Republic of China, located to the margin of Zhunger Basin(Jurassic Formation Ð oil and gas bearing layer, oil and gas stored in overthruststructures). This oil field first time discovered by the local villagers, who found thatblack material on the surface and then known as asphalt.6. NEW LOOK TO THE AREABased on our study to the geological research history work, the neotectonicmovement, the new crust movement, and our interpretation for the satellite images,we have a new look to the area. This new look to the area depending on our newthinking, that during the successive rift phases, (The Karroo Rift Phase; The SomaliRift Phase; The Mascarene Rift Phase; The Yemen Rift Phase), the expected mainextensional faults trend and the minor extensional faults trends changed theirdirection.Especially, during the recent time, where we find that:1. The first type of faults, which has the NE-SW directions, is a normal and obliquenormal fault.2. The second type of faults, which has the EÐW and ENE-WSW directions, is adivergent sinistral wrench faults and has the same trend of the southern border of thedesert, which is also roughly the trend of the dune ridges.3. The third type of faults, which has the NÐS and NNE-SSW directions, is divergentdextral wrench faults.Note (4): The second type of faults and the third type of faults are a share faults type,with right and left hands.5. The forth type of faults, which has NWÐSE directions, is over thrust faults.CONCLUSION1. As a result of our study, we think that a new rift phase started in the area during therecent time.2. On this new rift phase:a. The first type of faults, which has the NE-SW directions, is a normal and obliquenormal fault. They are parallel to the direction of the largest principle stress of theArabian plate.b. The forth type of faults, which has NWÐSE directions, is over thrust faults. Theirextensional fault trend resulted by the largest principle stress of the Arabian plate.3. We think, that this new stage has the same main rift trends like the Karroo riftsphase (?).4. The natural asphalt (?) shown on the surface of this area by the satellite imagesmight be a very clue for looking for a new petroleum discoveries.RECOMMENDATION1. It is recommended that a very highly qualified team study the Yemeni sector ofRub al Khali basin for recognition of crustal zones of weakness, their trend and origin
  6. 6. is thus of vital importance in the interpretation of rift structures. We believe that thisarea, which took some care in the past and attracts many experts in the present time, isnot going just to surprise all with its oil and gas discoveries, but also with its very richgeological data in the future.2. The most important thing, that we want to drew the Ministry of Oil andMineral Resources, foreign companies and all who are interested in this area toconcentrate their exploration attention on the following two coordinate pointsand the adjacent area around them:First Point: N 18.46O / E 51.05OSecond Point: N 18.22O / E 49.67OREFERENCES:1. Beydoun, Z.R., As-Saruri, M.L., and Baraba, R.S., 1996. Sedimentary basins of theRepublic of Yemen: their structural evolution and geological characteristics. Revue deIInstit. Francais du Petrole, 51, No.6, Nov.-Dec. 1996.2. Bunker, D.G., 1953. The Southwest Borderlands of Rub al Khali: Geol. Jour. v. 19,pt. 4, p. 420-430.3. Dyer, R.A. and Husseini, M.I., 1991. The western Rub al-Khali Infracambriangraben system. Proceedings SPE Middle East Oil Show, Nov. 1991, Bahrain, 505-512(SPE 21396).4. Mills, S.J., 1992. Oil discoveries in the Hadhramaut: how Canadian OXY scored inYemen. Oil and Gas Journal, (9 March 1992), 49-52.5. Nani A.S.O., 1998. Miscellaneous Scientific Articles on geology and hydrocarbonexploration in Yemen (Flower Structure in the Yemeni Sector of the Rub al KhaliBasin and Paleozoic clastic reservoir in Oman, Saudi Arabia and Yemen).6. Nedham, M.Darsi, 2000. The Geological Research History Work in the Republic ofYemen during the period from 1852 until Today (Three papers). Yemen Timesnewspaper. Issue 2-January 10th through January 16 2000, Vol. IX, Culture Page,Issue 10 - March 6 through March 12 2000, Vol. X, Culture Page and Issue 15 - April10 through April 16 2000, Vol. X, Culture Page.7. Peter E. Putnam, George Kendall, and David A. Winter, 1997. Estuarine Depositsof the Upper Qishn Formation (Lower Cretaceous), Masila Block, Yemen. AAPGBulletin, V. 81, No.8 (August 1997), P. 1306-1329.8. The Columbia Encyclopedia, Fifth Edition Copyright ©1993, Columbia UniversityPress. Licensed from Inso Corporation.ABOUT THE AUTHOR* Wang Xikui graduated from Changchun University of Science and Technology in1982 and got his Doctor degree from Lanzhou Institute of Desert, the ChineseAcademy of Sciences in 1995. He studied and worked as a postdoctoral student inChangchun University of Science and Technology from 1997 to 1999. His scientificinterest is Concentrated on the neotectonic movement and petroleum resources,Quaternary Geology and geomorphological system modeling.** Mohammed Darsi graduated from the Russian among People FriendshipUniversity in 1991 as a Petroleum Engineer, Geologist (M.S. degree). He began hisprofessional career by working as petroleum engineer, geologist in the PetroleumExploration and Production Board (Aden Branch). His scientific interest isconcentrated on the Geological Research History Work, Earth science softwareapplication and basin-modeling problems.