首页> 外国专利> METHOD OF DETECTING AND MAPPING FLUID-SATURATED ANISOTROPIC CAVERNOUS-FRACTURE RESERVOIRS IN INTER-SALT CARBONATE FORMATIONS OF A SEDIMENTARY COVER

METHOD OF DETECTING AND MAPPING FLUID-SATURATED ANISOTROPIC CAVERNOUS-FRACTURE RESERVOIRS IN INTER-SALT CARBONATE FORMATIONS OF A SEDIMENTARY COVER

机译:沉积盖盐分碳酸盐岩地层中流体饱和各向异性的穴形-裂缝储层的探测与映射方法

摘要

FIELD: geophysics.;SUBSTANCE: invention relates to the field of seismic exploration and can be used for mapping of complex fluid-saturated fractured-cavernous zones, with AHPP of fluids in geologic section of sedimentary cover of platforms and areas of their connection with marginal troughs. During excitation and registration of seismic signal of CDPM, data are processed with maximum attenuation of interference and ensuring preservation of primary seismic field, with separation of scattered component. Besides, energy and spectral characteristics, as well as degree of irregularity of scattered component seismic signals are determined. According to abnormal values of said parameters, fracture-cavernous zones with different degree of fracturing and cavernousness are selected. Inter-salt fluid-saturated reservoirs are a special prediction object, the geological structure of which is fundamentally different from massive fracture reservoirs, and is therefore characterized by special effects of reflection and recording in the wave field.;EFFECT: improving reliability of prediction of complex fluid-saturated fractured-cavernous zones, with abnormally high bed pressure of fluids in halogen-carbonate sequences of geological section of sedimentary cover of platforms and areas of their connection with marginal troughs, which complicate drilling at different stages and stages of geological prospecting process.;1 cl, 6 dwg
机译:技术领域本发明涉及地震勘探领域,可用于绘制复杂的,流体饱和的裂隙-海绵状地层,平台沉积覆盖层的地质部分及其与边缘的连接区域的流体的AHPP槽。在CDPM地震信号的激励和记录过程中,对数据进行处理时会最大程度地减少干扰,并确保保留主要地震场,并分离分散的分量。此外,还确定了能量和频谱特性,以及散射分量地震信号的不规则程度。根据所述参数的异常值,选择具有不同程度的裂缝和海绵状的裂缝-海绵带。盐间饱和流体储层是一个特殊的预测对象,其地质结构与大型裂缝性储层根本不同,因此具有波场反射和记录的特殊作用。复杂的饱和流体裂缝-孔洞带,平台沉积覆盖层地质段及其与边缘槽相连的区域的卤代碳酸盐岩层序中的流体地层压力异常高,这使地质勘探过程的不同阶段和阶段的钻探变得复杂。; 1 cl,6 dwg

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