Depth structural mapping of syn and pre-rift rock units of southeast Ghara at southern end of Gulf of Suez

IF 2.1 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Osama Elghrabawy , Shaimaa Abd El Raheem , Alaa Aref , Khaled Khalifa
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Abstract

The interpretation of seismic data in the Gulf of Suez area for identifying and imaging pre-Miocene horizons is problematic due to the influence of thick evaporites near the surface. Consequently, this paper sheds light on the imaging of shallow and deep structure complexity of southeast Ghara based on an integrated analysis of seismic and aeromagnetic data. The analysis strategy included in-depth structural mapping of syn and pre-rift formations. The results indicate that the Miocene and pre-Miocene structure complexities are related to southwest-dipping blocks controlled by major listric faults associated with dip-slip faults. These structures are considered the main cause of forming the tilted faulted blocks in the study area, with a trend NNW to NW and many cross faults in ENE and NE in the study area with NNW to NW trends and many cross faults in the ENE and NE directions. One of these tilted faulted blocks forms the main horst structure trend in the Ghara area. The depth structure maps show that the depths of formations increase gradually westward and decrease eastward. The sub-basins in the western part exhibit an average thickness of 5029 m and are bounded by a salt ridge in the southeast and the uplifted offshore basement in the northwest. The lowermost portions of the Miocene formations and the pre-rift strata thickness are identified by mapping the basement and the base of the Rudeis Formation, which exhibit an average thickness of 549 m. The structure complexity analysis shows probable locations to entrap and accumulate hydrocarbons. The interpretation suggests that the up-thrown side of the interpreted normal faults show promising locations for hydrocarbon accumulations, especially along the central to southern, and northern portions of the Ghara study area.
苏伊士湾南端加拉东南同裂谷前岩单元深度构造填图
由于地表附近厚的蒸发岩的影响,苏伊士湾地区用于识别和成像前中新世地层的地震数据解释存在问题。因此,本文在综合分析地震和航磁资料的基础上,阐明了塔里木盆地东南部浅部和深部构造复杂性的成像方法。分析策略包括对同步地层和前裂谷地层进行深入的构造作图。研究结果表明,中新世和前中新世构造复杂性与受倾斜断裂控制的西南倾断块有关。这些构造被认为是研究区倾斜断块形成的主要原因,研究区以NNW - NW走向为主,以NNW - NW走向为主,以ENE - NE向为主,以ENE - NE向为主。其中一个倾斜断块形成了格拉地区主要的主构造走向。深度构造图显示,地层深度向西逐渐增大,向东逐渐减小。西部次盆地的平均厚度为5029 m,东南部为盐脊,西北部为隆升的近海基底。通过对鲁德斯组基底和基底的测绘,确定了中新世组的最下部和裂谷前地层厚度,平均厚度为549 m。构造复杂性分析显示了油气可能成藏和聚集的位置。解释表明,正断层的上倾面显示出油气聚集的有利位置,特别是在Ghara研究区的中部至南部和北部。
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来源期刊
Journal of Applied Geophysics
Journal of Applied Geophysics 地学-地球科学综合
CiteScore
3.60
自引率
10.00%
发文量
274
审稿时长
4 months
期刊介绍: The Journal of Applied Geophysics with its key objective of responding to pertinent and timely needs, places particular emphasis on methodological developments and innovative applications of geophysical techniques for addressing environmental, engineering, and hydrological problems. Related topical research in exploration geophysics and in soil and rock physics is also covered by the Journal of Applied Geophysics.
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