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遥感油气勘探对伊犁盆地的评价 总被引:3,自引:0,他引:3
遥感油气勘探技术是通过遥感影像的构造解译及烃类微渗漏信息的提取并结合其他地质资料,对目标区进行油气有利聚集区的预测及评价。利用这一勘探技术着重对伊犁盆地的构造特性、承压盆地、构造阶地、烃类微渗漏信息等进行了解译和提取,总结出伊犁盆地油气藏预测的九大要素,确定了3条油气聚集带和14个油气远景区。 相似文献
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晋陕地区地质构造演化与油气聚集 总被引:19,自引:0,他引:19
王同和 《华北地质矿产杂志》1995,10(3):283-398
区域构造演化研究对于搞清盆地构造层的数量、类型及其叠置方式,进而评价油气远景、估算储量、选区、勘探和深化对老区的认识并开拓油气新领域。新层系、新类型、新深度,以及探讨油气区的地球动力学等基本问题均具有重要的实际意义,作者就晋陕及周边地区的地质、地球物理、地球化学和钻井以及卫星影像等的实际资料,综合论述了本区的构造变动,岩浆活、沉积作用,成油过程、油气运移与聚集机制。以及油气藏时空分布规律和油气勘控 相似文献
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论羌塘盆地油气勘探前景 总被引:8,自引:0,他引:8
羌塘盆地与中东油气区同属于特提斯构造域,是我国陆上新区面积最大的海相盆地。近20年来,我国油气地质工作者在条件极其艰苦的藏北高原开展了系统的油气地质调查和研究工作,完成了从含油气盆地分析到资源潜力评价、战略选区、靶区预测、井位论证及实施科探井的全过程,获得了一系列新发现和新认识,提出了羌塘盆地是我国最有希望取得突破的油气勘探新区。但是,对上述认识也还存在不同的看法,特别是对油气保存条件和盆地生烃潜力,还存在“好”与“不好”两种截然不同的观点。本文根据最近完成的羌塘盆地科探井工程(羌科 1井)及其配套的地质—地球物理工作所取得的最新资料,结合近20年来羌塘盆地油气地质调查所取得的成果,重点围绕烃源岩与保存条件这两个方面,对羌塘盆地油气地质特征进行论述,力求客观、准确评价羌塘盆地油气保存条件,同时分析、预测了盆地生烃潜力及油气远景,并提出下一步油气勘探建议,以期持续推进羌塘盆地未来油气勘探工作,早日实现盆地油气勘探重大突破。 相似文献
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《吉林大学学报(地球科学版)》2006,36(3):479-479
《大庆探区外围中、新生代断陷盆地群演化与油气远景》(项目编码XQ-2004-07)由吉林大学承担。项目的任务是研究大庆探区外围中、新生代盆地形成的区域大地构造背景、盆地类型及其演化规律;查明大庆探区外围中、新生代断陷盆地群的油气潜力,优选有利勘探战略目标区。工作区包括内蒙古自治区的东北部、黑龙江省和吉林省的东部地区,总面积约130万km^2,涉及大庆探区外围面积大于1600km^2的盆地共14个, 相似文献
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Saeed Waleed Shouakar-Stash Orfan Unger André Wood Warren W. Parker Beth 《Hydrogeology Journal》2021,29(5):1939-1951
Hydrogeology Journal - Sabkha Matti is a potential discharge point for regional groundwater systems in the Rub’ al Khali topographic basin of Saudi Arabia. The hydrogeochemical evolution of... 相似文献
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沙特鲁卜哈里盆地Unayzah组是中东地区重要的含油气层位,野外地质调查研究和钻井地质研究的结果表明,Unayzah组的沉积环境是在干旱条件下沉积的风成沙丘、干盐湖、季节性辫状河流以及风化壳。由于Unayzah组砂岩中石英含量比较高,岩石类型主要为石英砂岩,成岩作用较为简单,成岩作用对储层的改造和影响比较小。储集空间类型主要为粒间孔隙。Unayzah组是鲁卜哈里盆地油气勘探的主要目的层。 相似文献
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Sand and dust storms are causing hazards and problems in aviation as well as the dangers and distresses they cause on living things. The low meteorological visibility, the presence of strong winds with gust, and the transport of dust and sand particles by the wind are dangerous on landing and departure of aircrafts, and even on planes that are parked. The main aim of the study is to examine the meteorological conditions causing the dust storm that took place in the Arabian Peninsula on February 28, 2009, and to determine the source of dust caused dust storm, sand storm, blown sand, and blown dust at the airports. Within the scope of the study, aviation routine weather report (METAR) and aviation selected special weather report (SPECI) reports have been assessed at many airports over Arabian Peninsula (AP), the northern part of the AP and North Africa. As model outputs; NCEP–DOE Reanalysis 2 data, BSC–DREAM8B, and HYSPLIT model were used. In the satellite images; METEOSAT MSG dust RGB images, MODIS, and Kalpana-1 data were used. According to obtained results, dust storms were detected in Bahrain, Kuwait, Saudi Arabia, and United Arab Emirates (UAE). At Al-Ahsa Airport in Saudi Arabia, the lowest visibility measured on February 28, 2009, dropping to 200 m, which was dominated by blowing sand. The source region of the dust observed at Dubai Airport in UAE is the eastern regions of the Rub’al Khali Desert located between Saudi Arabia, Oman, and UAE. 相似文献
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Warren W. Wood 《Hydrogeology Journal》2011,19(1):155-161
Paleo-groundwaters of 6000?years BP from the Liwa water-table sand dune aquifer in the Rub al Khali and the Gachsaran artesian carbonate aquifer, on the coast of the Emirate of Abu Dhabi (UAE), exhibit normal ??2H/??18O slopes, modest ??18O increases, and large negative deuterium excess ??d?? (Liwa aquifer: 2.19?? VSMOW and d?=??C15; Gachsaran aquifer: 3.16?? VSMOW and d?=??C28) compared to local Shamal precipitation (0.05?? VSMOW and d?=?7). This unusual isotopic signature is hypothesized to result from re-evaporation of continental runoff to the Red Sea catchment basin. It is postulated that this continental water flowed onto the surface of the Indian Ocean providing a moisture source for the monsoon that dominated precipitation during this, the last wet period in the area from 5000 to 9000 BP. Carbonate precipitation, forming speleothems, travertines, tufas, lacustrine, and capillary-zone deposits, subsequently record this ??18O isotopic signature. This rock record is thus dominated by the water source, rather than environmental conditions of deposition normally assumed to control the rock ??18O isotopic signature. As a consequence, re-evaluation of paleo-climate??18O data from the rock record may be necessary for this time period in southern Arabia. 相似文献
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Miško Milanović Milisav Tomić Veljko Perović Milan Radovanović Saumitra Mukherjee Darko Jakšić Marko Petrović Ana Radovanović 《Environmental Earth Sciences》2017,76(16):580
This paper presents the effect of land-use changes on land degradation by utilization of remote sensing methods and the Gavrilovi? erosion potential method, due to surface mining activities in the period 2001–2011. Studied area includes the zone of influence of the Rudarski basen Kolubara, which covers the exploitation area of the Kolubara coal basin in the Republic of Serbia. The analysis is based on the processing of Landsat 5 satellite images from 2001 and 2011. In the analysis of satellite images, the supervised classification method was used. The results suggest that the observed spatial–temporal area is exposed to erosion as a result of land-use changes. Preliminary conclusion is that the dominant anthropogenic factor, responsible for changes in land use, is pronounced through the mining activity, industrialization, construction as well as agricultural activities. Very small changes in land use that occurred in the period 2001–2010 have led to relatively small amount of change from the aspect of land degradation. Also, due to the planned exploitation of the mine which included into account the sustainability of ecosystems, primarily through appropriate conservation measures, RB Kolubara is not in danger of a possible erosion processes that could undermine the stability of the basin. 相似文献
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Abderrazak El Harti Abderrazak Bannari El Mostafa Bachaoui El Mostafa Aarab Guillaume Girouard Abderrahmen El Ghmari 《Comptes Rendus Geoscience》2004,336(14):1311-1320
The geodynamic model of the Palaeozoic basin opening of central Jebilet has been unknown before this study in spite of the abundance in the geological studies carried out in the studied sector using conventional methods. This is due to the scarcity of the key beds and synsedimentary structures. Using the synergy between the image data of the Landsat satellite TM sensor and the ground data, we have highlighted, herein, new structural data allowing the design of a new model of the Palaeozoic basin opening of central Jebilet. This opening could have been made according to dextral submeridian transverse faults with the individualization of subequatorial normal faults. To cite this article: A. El Harti et al., C. R. Geoscience 336 (2004). 相似文献
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Effects of mining subsidence on masonry buildings in Zonguldak hard coal region in Turkey 总被引:5,自引:4,他引:1
Gallerias are the underground constructed results of mining. As these space in underground layers collapse, horizontal and vertical ground movements occur and movement which may reach the earth’s surface are known as mining subsidence. The result of underground displacement may cause surface ground movement which can be detrimental to masonry buildings especially in hard coal regions. Thorough familiarity with general and regional characteristics of an affected area can assist reduction of the effects. Zonguldak and the nearby settlement area, with a population of 300,000, constitute the centre of a hard coal basin where extensive mining has a history extending through 160 years. Mining constitutes the main economic activity in this region, and consequently influences every aspect of life. This study’s intent is to identify the effects of mining subsidence on masonry buildings in the mining area of Kozlu, Zonguldak, Turkey and illustrate them with selected images of damaged masonry buildings. Also included are satellite and mining galleria images. 相似文献
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G Nageswara Rao 《Journal of Earth System Science》2001,110(1):87-94
It is well known that heavy rainfall occurs in the southwestern sector of the monsoon depressions due to strong convergence
in that sector. By examining the rainfall distribution associated with the monsoon disturbances (lows and depressions) in
one of the central Indian river basins, ‘Godavari’, the author found that when the disturbance-centre is away from the basin,
heavy rainfall may also occur in the basin area close to the confluence line and cause severe floods in the river. The confluence
line is the zone of convergence between the northeasterlies to the west of the disturbance centre and the monsoon westerlies.
This study further reveals the importance of the position and movement of the confluence line with respect to the basin, on
which the intensity and the raising period of the resulting flood depend. 相似文献