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    • 3. 发明申请
    • AREAL MONITORING USING DISTRIBUTED ACOUSTIC SENSING
    • 使用分布式声学感测进行AREAL监测
    • WO2010090660A1
    • 2010-08-12
    • PCT/US2009/060767
    • 2009-10-15
    • SHELL OIL COMPANYSHELL INTERNATIONALE RESEARCH MAATSCHAPPIJ B.V.LOPEZ, Jorge LouisWILLS, Peter Berkeley
    • LOPEZ, Jorge LouisWILLS, Peter Berkeley
    • G01V1/28G01V1/22G01V1/16
    • G01V8/16E21B47/102
    • A method for obtaining seismic information about a subsurface formation using at least one fiber optic cable having its proximal end coupled to a light source and a photodetector comprises: transmitting into the cable at least one light pulse; receiving at the photodetector a first and second light signals indicative of the physical status of at least one first cable section and at least one second cable section, respectively, wherein the first and second sections are selected so as to provide first and second information items, respectively; optionally, further processing at least one of the first and second information items so as to produce derivative information; and outputting at least one of the first, second, and derivative information items to a display; wherein the second item differs from the first item in at least one aspect selected from the group consisting of: resolution, area, and location.
    • 一种用于使用至少一根光纤电缆获得关于地下地层的地震信息的方法,所述至少一根光缆具有耦合到光源的近端和光电检测器,包括:将至少一个光脉冲传输到所述电缆; 在光电检测器处接收分别指示至少一个第一电缆部分和至少一个第二电缆部分的物理状态的第一和第二光信号,其中选择第一和第二部分以便提供第一和第二信息项, 分别; 可选地,进一步处理第一和第二信息项中的至少一个,以产生导数信息; 并将第一,第二和导出信息项中的至少一个输出到显示器; 其中所述第二项目与至少一个方面中的所述第一项目不同,所述方面从由以下组成的组中选择:分辨率,面积和位置。
    • 8. 发明申请
    • METHOD OF AND SYSTEM FOR CREATING A SEISMIC PROFILE
    • 创建地震剖面的方法和系统
    • WO2016106278A1
    • 2016-06-30
    • PCT/US2015/067270
    • 2015-12-22
    • SHELL OIL COMPANYSHELL INTERNATIONALE RESEARCH MAATSCHAPPIJ B.V.
    • MATEEVA, Albena AlexandrovaWILLS, Peter BerkeleyLOPEZ, Jorge LuisHORNMAN, Johan Cornelis
    • G01V1/02G01V1/42
    • G01V1/42G01V1/02G01V2210/1299
    • A seismic source (50) is buried in a multi-layered subsurface formation below a fast layer (30) and above a reflecting interface (10). The seismic source (50) excites a critically refracted (CR) wave that travels laterally along a fast layer bottom interface (35), and emanates downwardly into a slow layer (40) that is below and adjacent to the fast layer (30). One or more receivers (60), positioned below the fast layer (30) and above the reflecting interface (10) are used to detect seismic waves (84, 86). The one or more receivers (60) are positioned within a borehole (65). At least one reflected CR wave is isolated from the received signals, which is a CR wave that has reflected off of the reflecting layer (10) below the one or more receivers (60). A seismic profile of the multi-layered subsurface formation is created, using the at least one reflected CR wave. Time-lapse seismic monitoring of hydrocarbon extraction operations, such as steam injection, is also provided.
    • 地震源(50)被埋在快速层(30)下面和反射界面(10)之上的多层地下地层中。 地震源(50)激发沿着快速层底界面(35)横向传播的重折射(CR)波,并且向下发射到位于快速层(30)下方并邻近快速层(30)的缓慢层(40)。 位于快速层(30)下方和反射界面(10)下方的一个或多个接收器(60)用于检测地震波(84,86)。 一个或多个接收器(60)定位在钻孔(65)内。 至少一个反射CR波与接收信号隔离,所接收的信号是从一个或多个接收器(60)下面的反射层(10)反射的CR波。 使用至少一个反射CR波形来创建多层地下地层的地震剖面。 还提供了对蒸汽注入等烃类提取操作进行延时地震监测。