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Geological studies of the coastal area between Mersa um Gheig and Ras Banas , RedSea coast, Egypt

机译:埃及红海沿岸Mersa um Gheig和Ras Banas之间沿海地区的地质研究

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Egypt's Red Sea coast runs from the Gulf of Suez to the Sudanese border. The length of the study area between Mersa um Gheig and Ras Banas is about 240 km. The main geomorphological unit in the study area includes mountains (basement), shoreline, beach, alluvial fan, and flood plain. The study area studied by tow methods: 1- sedimentological and mineralogical (Geologic) methods 2- remote sensing methods. The geologic method give a light picture about the composition of the beach, where the beach sediments range from calcareous sand in the north of the study area (Mersa um Gheig, the sand percent 86.83%) to carbonate beach in the south of the study area (Ras Banas, the carbonate percent 96.78%). Also the heavy minerals in the beach sand studied in fine (0.250-0.125mm) and very fine(0.125 – 0.063mm) fractions (average percentages of two fractions) to shed more light on the nature of the source rocks and their sedimentary history. Opaques and non Opaques (Amphibole, Epidote, staurolite, Zircon, Muscovite, Chlorite, Garnet, Rutile) are studied in detail as averages in both fine and very fine fractions. The heavy metals (elements) in the study area estimated and interpreted, where, Ba range from 10.1 to 315 ppm, Sr range from 548 to 2800 ppm, Cr range from 0.0 to 250 ppm, , Ni range from 0.0 to 103ppm, Cu from 10 to 35ppm, Zn from 0.0 to 94 ppm, Sc from 0.0 to 17.6 ppm, V from 0.0 to 277 ppm, Y from 0.0 to 9ppm, and Mo from 2 to 16 ppm. The remote sensing method also used in this area for study the sedimentation changes in many selected sites. Finally the purpose of this study is determination the geological and environmental properties of each beach in the selected sites and the suitable of each site for different sustainable development activities.
机译:埃及的红海海岸从苏伊士湾一直延伸到苏丹边界。研究区域的长度介于Mersa um Gheig和Ras Banas之间,约为240公里。研究区域的主要地貌单位包括山脉(地下室),海岸线,海滩,冲积扇和洪泛平原。通过拖曳方法研究的研究区域:1-沉积学和矿物学(地质)方法2-遥感方法。地质方法可以清晰地描述海滩的组成,其中海滩沉积物的范围从研究区域北部的钙质砂(Mersa um Gheig,砂百分比为86.83%)到研究区域南部的碳酸盐海滩(拉斯巴纳斯,碳酸盐百分比为96.78%)。另外,对沙滩砂中的重矿物进行了细碎(0.250-0.125mm)和非常细碎(0.125 – 0.063mm)(两个碎屑的平均百分比)的研究,以进一步阐明烃源岩的性质及其沉积历史。不透明和非透明(闪石,埃皮多德,星光石,锆石,白云母,绿泥石,石榴石,金红石)均以细级和极细级的平均值进行了详细研究。对研究区域中的重金属(元素)进行了估算和解释,其中Ba的范围为10.1至315 ppm,Sr的范围为548至2800 ppm,Cr的范围为0.0至250 ppm,Ni的范围为0.0至103ppm,Cu的范围为10至35ppm,Zn为0.0至94ppm,Sc为0.0至17.6ppm,V为0.0至277ppm,Y为0.0至9ppm,和Mo为2至16ppm。该地区也使用遥感方法研究许多选定地点的沉积变化。最后,本研究的目的是确定选定地点中每个海滩的地质和环境特性,以及每个地点是否适合不同的可持续发展活动。

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