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| 1 | Huff ’n puff to revaporize liquid dropout in an Omani gas field显示文摘 | M. Al-Wadhahi F.H. Boukadi A. Al-Bemani R. Al-Maamari H. Al-Hadrami | 2006 | Journal of Petroleum Science and Engineering2006，，1： | 1 |
| 2 | Characterization of paraffinic deposits in crude oil storage tanks using high temperature gas chromatography显示文摘 | Boukadi A Philp R P Thanh N X | | 0，，10： | 1 |
| 3 | The evolution of pre-existing structures during the tectonic inversion process of the atlas chain of tunisia显示文摘 | Dhahri F Boukadi N | | 0，，： | 1 |
| 4 | Threshold Pressure as a Measure of Degree of Rock Wettability and Diagenasis in Consoledated Omani Limestone Cores 显示文摘 | Boukadi F Bemani A Rumhy Ivi | 1998 | Mar Petrol Geol1998，15，： | 1 |
| 5 | A comparativestudy of lost circulation materials显示文摘 | BOUKADI F YAGHI B AL-HADRAMI H | 2004 | Energy Sources2004，26，10： | 1 |
| 6 | Geochemical Record of the Cenomanian-Turonian Anoxic Event in Tunisia:Is it Correlative and Isochronous to the Biotic Signal?显示文摘在突尼斯,五 Bahloul spaced 节, Bargou, Jerisa, Guern Halfaya, Kherij 和 Gafsa 为 biostratigraphy (有孔虫类和放散虫类的各类动物) 被分析并且主修并且跟踪元素。这高分辨率的 biostratigraphic 和 chemostratigraphic 综合分析为迟了 Cenomanian 早 Turonian Bahloul 形成提供新卓见进南部的 Tethyan 边缘的 palaeoceanographic 进化。相对低许多联系了源自陆地的 Ti/Al 和 K/Al 比率和象 Ba , Cu ,和 Ni 那样的一些生产率代理的丰富(有机物联系了踪迹元素)建议 Bahloul ,在一个相对短的时期( 0.5 妈)期间扔了,具有相对提高的主要生产率和最小的由岩屑形成的输入。当时更高的 D * 与更低的 Ti/Al 比率并发的价值是由提高的河的材料贡献引起了被解释,由于更多的潮湿的气候在 OAE-2 期间。提高的湿度触发了可能河的流入,导致了懒惰的水发行量和在底部赞成有机物的保藏的作为结果的 anoxic/euxinic 条件。在在 Bahloul 形成存款和氧化还原作用的氧化还原作用敏感的踪迹金属 U , V ,和瞬间的丰富索引,例如V/( V+Ni ), U/Th , V/Cr ,和 Ni/Co ,显示限制氧的条件与相对许多在迟了的 Cenomanian 期间占优势到最早的 Turonian 时间和相互关联很好有孔虫目的一些和放散虫类的各类动物paleo环境的相关指示物。高 Baxs 价值和 Uauth 可以在 Bahloul 形成免职期间至少在 watersediment 接口显示缺氧的条件并且提供信息关于对中等硫酸盐减小反应低。 | Mohamed SOUA Dalila ZAGHBIB-TURKI Hela BEN JEMIA Jalel SMAOUI Amel BOUKADI | 2011 | Acta Geologica Sinica(English Edition)2011，85，6： | 1 |
| 7 | Aptian–Albian Transition in Central Tunisia:Tectonosedimentary and Paleogeographic Records显示文摘The Aptian–Albian series are characterized, in Tunisia, by several variations in subsidence rates and records discrete unconformity between Albian and Aptian in central and southern Tunisia. In central Tunisia Upper Aptian regressions were sustained until the beginning of Albian with a low sea level stand. In this paper, wells data gathered from central Tunisia exposes well expressed Aptian–Albian hiatus associated to several partial sedimentary gaps, erosion surface and unconformities and correlated with the 'Aptian Crisis' highlighted at the Tethyan scale. This latter is coeval with an extensional regime in concurrence with the African rifting responsible for halokinesis movements and magmatism and leaded to the establishment of paleoreliefs as much as tilted blocks and half grabens in central Tunisia. Deposition shows regional hiatus and lateral transition from platform facies to south to, open marine facies to the north. The structural configuration of this domain within normal faulting, horsts and grabens leaded to the establishment of several distinct basins with different subsidence rates. Discordances occur specially around and upward uplifted blocks and emerged land and are especially associated with Aptian reef, karsts and shallow marine facies. They are unconformably overlaid by the transgressive open marine facies of Albian–Cenomanian series acknowledged as source rock in Central Tunisia. In addition, the reefal Aptian facies is considered a potential reservoir rocks in central Tunisia and it is frequently associated to mineralization and Hydrocarbure reservoirs. | Imen Marco Ferid Dhahri Taoufik Haji Noureddine Boukadi | 2014 | Journal of Earth Science2014，25，5： | 0 |
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