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首页> 外文期刊>NRIAG Journal of Astronomy and Geophysics >Integration of seismic interpretation and petrophysical studies on Hawaz Formation in J-field NC-186 concession, Northwest Murzuq basin, Libya
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Integration of seismic interpretation and petrophysical studies on Hawaz Formation in J-field NC-186 concession, Northwest Murzuq basin, Libya

机译:利比亚西北穆尔祖克盆地J油田NC-186特许权的哈瓦兹组地震解释与岩石物理研究相结合

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This study has been carried out by the integration of seismic interpretations and the well-logging analysis of ten wells distributed in J-field of concession NC-186, Murzuq basin, Libya. Twenty (3D) seismic lines and ten wells have been analyzed. The results of this study indicated that, the main reservoir in this concession is Hawaz Formation. Hawaz has been split into 8 units with a subdivision of Hawaz H4 into three subunits with the objective of better characterization of the three general fine upward intervals. The lower interval of H4 zone presents the better reservoir properties. The depth of reflector H4 ranges from 4100 ft in the northwestern part of the study area and increases to 4600 ft in the southeastern part of the study area. In this study, the outline of the Hawaz paleohighs which is NC-186 Field “J” is generally trending in the NW-SE direction. The well logging analysis particularly quick look interpretation indicates that Hawaz Formation in the studied wells is mainly oil-bearing with some water-bearing sand levels at the horizons from H4 to and H6 which are potentially the main reservoirs. The water bearing zones are beyond these horizons starting from the sub-horizon H6c and the oil water contact is probably at depth 4495 ft. The crossplot of porosity-saturation for H5 and H6b indicates firmly that these horizons are indeed at irreducible state and will produce mainly oil as indicated in J4-NC186 well, while the crossplot of H8 shows wide scattering of points which is the main characteristic for water producing horizon. The depth of Hawaz Formation H4 is more than 4160 ft in J4, J12 and J16 wells in the northwestern parts of this field and increases to 4400 in the central part of the concession at well J1.
机译:这项研究是通过整合地震解释和对利比亚Murzuq盆地NC-186特许J井中分布的10口井的测井分析进行的。分析了二十条(3D)地震线和十口井。研究结果表明,该区块的主要储层为哈瓦兹组。 Hawaz已被分为8个单元,将Hawaz H4细分为三个子单元,目的是更好地表征三个常规的精细向上间隔。 H4带的间隔越小,储层特性越好。反射器H4的深度在研究区西北部的4100英尺范围内,并在研究区东南部的4600英尺处增加。在这项研究中,Hawaz古高地的轮廓线是NC-186场“ J”,通常沿NW-SE方向发展。测井分析特别是快速的外观解释表明,研究井中的Hawaz组主要是含油的,在H4至H6的地平线上有一些含水砂层,这可能是主要的储层。从次地平线H6c开始,含水层超出了这些视界,并且油水接触可能在4495英尺深处。H5和H6b的孔隙度饱和交会图明确表明,这些视界确实处于不可还原状态,并且会产生如J4-NC186井所示,主要为石油,而H8的交会图显示了点的广泛散射,这是产水层位的主要特征。在该油田西北部的J4,J12和J16井中,Hawaz组H4的深度超过4160 ft,在J1井特许权的中部增加至4400 ft。

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