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Thinly Bedded Reservoir Characterization, from Qualitative to Quantitative Approach, Case Studies in a Cenozoic Basin of Malaysia

机译:较薄的储层储层表征,从定性到定量方法,马来西亚新生代盆地的案例研究

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The limit of resolution of seismic data is a complex issue that involves not only wavelet frequency, phase characters, data quality (S/N), interference, tuning, but also criteria on how to measure resolvability, which can hamper confident lithology, porosity and fluid prediction of thinly bedded reservoirs. Widess's classic paper (1973) concluded that for thin beds (belowλ/8 wavelength), the seismic character, peak/trough time and frequency do not change appreciably with thickness, and also amplitude varies almost linearly with thickness, which goes to zero at zero thickness. Thus, λ/8 of wavelength is considered to be the fundamental limit of vertical seismic resolution which depends on velocity and mainly frequency. Tirado's work (2004) revised Widess's model, which is not applicable to the real reflection, and concluded that as the bed thickness decreases, there is a gradual increase in the peak frequency, but below a certain thickness (at some fraction of tuning thickness), the peak frequency rolls off and return to the peak frequency of the wavelet at zero thickness. Thus, the key factor in determining seismic resolution is by enhancing the frequency spectral bandwidth which, nowadays, can be effectively achieved either by acquiring Broadband Acquisition or conducting Broadband Seismic Re-Processing. We demonstrated various case studies on thinly bedded reservoirs using qualitative and qualitative techniques in a Cenozoic basin in Malaysia. The qualitative techniques involve the-90°Phase wavelets with Relative Colored Inversion, Spectral Decomposition, and ThinMAN broadband spectral inversion. The quantitative approach includes an integrated multi- disciplinary technique combining with Cascading AVO Simultaneous inversion and Stochastic Inversion calibrated with conventional and SHARP-OBMI logs, which together, significantly enhance imaging of the thinly bedded reservoirs. This unique integrated workflow has been applied in the field study, resulting in an increase of about 30% of hydrocarbon in-place volume, and has been successfully validated with available production/well data as well as newly drilled wells.
机译:地震数据的极限是一个复杂的问题,不仅涉及小波频率,相位字符,数据质量(S / N),干扰,调整,以及如何测量可解义的标准,这可能妨碍自信的岩性,孔隙度和孔隙度薄层玻璃储层的流体预测。 Widess的经典纸(1973)得出结论,对于薄床(低于λ/ 8波长),地震性质,峰值/槽时和频率不会明显地变得明显,厚度几乎线性变化,厚度几乎不同,厚度为零厚度。因此,波长的λ/ 8被认为是垂直地震分辨率的基本极限,这取决于速度和主要频率。 Tirado的工作(2004)修改了Widess的型号,这是不适用于真正的反射,并且得出结论认为随着床厚度的降低,峰值频率逐渐增加,但低于一定的厚度(在一定的调谐厚度上) ,峰值频率滚动并返回到零厚度的小波峰值频率。因此,确定地震分辨率的关键因素是通过增强频谱带宽来通过获取宽带获取或进行宽带地震重新处理来有效地实现现在可以有效地实现的。我们在马来西亚中生成盆地中使用定性和定性技术展示了各种案例研究。定性技术涉及-90°相色波,具有相对彩色反转,光谱分解和薄宽带光谱反转。定量方法包括一种集成的多学科技术,其与级联AVO同时反转和随机反演的随机校准,与常规和夏普-OBMI日志一起校准,它们在一起,显着增强了薄层玻璃储存器的成像。这种独特的集成工作流程已应用于现场研究,导致碳氢化合物的较高量增加约30%,并已成功验证,可用生产/井数据以及新钻井井。

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