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    • 1. 发明申请
    • METHOD OF AND SYSTEM FOR RECORDING SEISMIC SIGNALS
    • 记录地震信号的方法和系统
    • WO2016123015A1
    • 2016-08-04
    • PCT/US2016/014712
    • 2016-01-25
    • SHELL OIL COMPANYSHELL INTERNATIONALE RESEARCH MAATSCHAPPIJ B.V.
    • HORNMAN, Johan CornelisMATEEVA, Albena AlexandrovaLOPEZ, Jorge Luis
    • G01V1/42
    • G01V1/003G01V1/42
    • A first stationary seismic receiver array is provided in a first non-vertically directed first borehole section of a first array of non-vertically directed first borehole sections, and a second stationary seismic receiver array is provided in a second non-vertically directed first borehole section of the first array of non-vertically directed first borehole sections. A seismic source assembly is moved axially through a first non-vertically directed second borehole section from at least a first position to a second position of a plurality of first borehole positions along a length of the first non-vertically directed second borehole section. The seismic source assembly contains a repeatable seismic source, which is activated when the seismic source assembly is in the first position and when the seismic source assembly is in the second position. First and second shots of seismic signals are recorded with at least each of the first and second stationary seismic receivers.
    • 第一静止地震接收器阵列设置在第一非垂直定向的第一井眼部分阵列的第一非垂直定向的第一钻孔部分中,并且第二静止地震接收器阵列设置在第二非垂直定向的第一钻孔部分 的第一阵列的非垂直定向的第一井眼段。 地震源组件沿着第一非垂直定向的第二钻孔部分的长度沿第一非垂直定向的第二钻孔部分从至少第一位置移动到多个第一钻孔位置的第二位置。 地震源组件包含可重复的地震源,当地震源组件处于第一位置时,以及当地震源组件处于第二位置时,其被激活。 地震信号的第一次和第二次拍摄记录有至少每个第一和第二静止地震接收器。
    • 3. 发明申请
    • METHOD OF BOREHOLE TIME-LAPSE MONITORING USING SEISMIC WAVES
    • 利用地震波进行钻孔时间延迟监测的方法
    • WO2018084984A1
    • 2018-05-11
    • PCT/US2017/055143
    • 2017-10-04
    • SHELL OIL COMPANYSHELL INTERNATIONALE RESEARCH MAATSCHAPPIJ B.V.
    • MATEEVA, Albena AlexandrovaZWARTJES, Paul Maarten
    • G01V1/30G01V8/16
    • Receiver-consistent scalars of seismic receiver channels are used for time-lapse monitoring of a sub-surface earth formation. Signals are induced by seismic waves propagating through the earth formation adjacent to each respective seismic receiver channel. Each seismic receiver channel is acoustically coupled to the earth formation as present directly adjacent to the location of the seismic receiver channel in question. The base receiver-consistent scalars and the monitor receiver-consistent scalars of seismic receiver channels can be outputted to reveal changes in these receiver-consistent scalars. These changes can be used to delineate information about physical changes in the subsurface earth formation. The changes in the based receiver-consistent scalars and the monitor receiver-consistent scalars may be displayed visually.
    • 地震接收器通道的接收机一致标量用于地下地层的时间推移监测。 信号由传播通过邻近每个相应地震接收器通道的地层的地震波引发。 每个地震接收器通道在与所讨论的地震接收器通道的位置直接相邻的地方声学耦合到地层。 可以输出地震接收机通道的基准接收机一致标量和监测接收机一致标量以揭示这些接收机一致标量的变化。 这些变化可以用来描述有关地下地层中物理变化的信息。 可以直观地显示基于接收机一致的标量和监视接收机一致标量的变化。
    • 4. 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。