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    • 1. 发明授权
    • Method for determining positions of sensor streamers during geophysical surveying
    • 测量地球物理测量中传感器拖缆位置的方法
    • US08582394B2
    • 2013-11-12
    • US13327404
    • 2011-12-15
    • Gustav Göran Mattias SüdowJon FalkenbergBengt Rickard Finnoen
    • Gustav Göran Mattias SüdowJon FalkenbergBengt Rickard Finnoen
    • G01V1/38
    • G01V1/3835
    • A method for determining geodetic position of at least one point on a geophysical sensor streamer towed by a vessel in a body of water includes determining geodetic positions of a plurality of locations along a first geophysical sensor streamer towed at a first depth in the body of water. A lateral offset is caused between the first geophysical sensor streamer and a second geophysical sensor streamer towed at a second depth in the body of water. A distance is measured between at least two selected points along the first geophysical sensor streamer and a selected point along the second geophysical sensor streamer. A depth is measured at at least one point along the second geophysical sensor streamer. A geodetic position is determined at a selected point along the second geophysical sensor using the depth measurement, a direction of the lateral offset and the measured distances.
    • 用于确定由水体在水体中拖曳的地球物理传感器拖缆上的至少一个点的大地测位置的方法包括确定沿着水体第一深度处拖曳的第一地球物理传感器拖缆的多个位置的大地测量位置 。 在第一地球物理传感器拖缆和在水体中的第二深度处拖曳的第二地球物理传感器拖缆之间产生横向偏移。 在沿着第一地球物理传感器拖缆的至少两个选定点和沿着第二地球物理传感器拖缆的选定点之间测量距离。 在沿着第二个地球物理传感器拖缆的至少一个点处测量深度。 使用深度测量,横向偏移的方向和测量的距离,沿着第二地球物理传感器的选定点确定测地位置。
    • 5. 发明申请
    • METHOD FOR DETERMINING POSITIONS OF SENSOR STREAMERS DURING GEOPHYSICAL SURVEYING
    • 确定地球物理测量过程中传感器流体位置的方法
    • US20130155807A1
    • 2013-06-20
    • US13327404
    • 2011-12-15
    • Gustav Göran Mattias SÜDOWJohn FALKENBERGBengt Richard FINNOEN
    • Gustav Göran Mattias SÜDOWJohn FALKENBERGBengt Richard FINNOEN
    • G01V1/38
    • G01V1/3835
    • A method for determining geodetic position of at least one point on a geophysical sensor streamer towed by a vessel in a body of water includes determining geodetic positions of a plurality of locations along a first geophysical sensor streamer towed at a first depth in the body of water. A lateral offset is caused between the first geophysical sensor streamer and a second geophysical sensor streamer towed at a second depth in the body of water. A distance is measured between at least two selected points along the first geophysical sensor streamer and a selected point along the second geophysical sensor streamer. A depth is measured at at least one point along the second geophysical sensor streamer. A geodetic position is determined at a selected point along the second geophysical sensor using the depth measurement, a direction of the lateral offset and the measured distances.
    • 一种用于确定由水体在水体中拖曳的地球物理传感器拖缆上的至少一个点的大地测位置的方法,包括沿着在水体中的第一深度处拖曳的第一地球物理传感器拖缆确定多个位置的大地测位置 。 在第一地球物理传感器拖缆和在水体中的第二深度处拖曳的第二地球物理传感器拖缆之间产生横向偏移。 在沿着第一地球物理传感器拖缆的至少两个选定点和沿着第二地球物理传感器拖缆的选定点之间测量距离。 在沿着第二个地球物理传感器拖缆的至少一个点处测量深度。 使用深度测量,横向偏移的方向和测量的距离,沿着第二地球物理传感器的选定点确定测地位置。
    • 8. 发明申请
    • Subsurface electromagnetic survey technique using expendable conductivity, temperature, and depth measurement devices
    • 使用消耗电导率,温度和深度测量装置的地下电磁勘测技术
    • US20120182017A1
    • 2012-07-19
    • US12930746
    • 2011-01-14
    • Rune Johan Magnus MattssonGustav Göran Mattias Südow
    • Rune Johan Magnus MattssonGustav Göran Mattias Südow
    • G01V3/00G06G7/48
    • G01V3/12Y02A90/344
    • A method for modeling conductivity distribution in a formation below a body of water includes measuring electromagnetic response of the formation with an electromagnetic survey system; measuring at least one of water conductivity, water dielectric constant, and water temperature with respect to depth in the water; generating an initial model of conductivity distribution of the formation; discretizing the measurements of at least one of water conductivity, water dielectric constant, and water temperature with respect to depth into at least one layer; generating a forward model of a response of the electromagnetic survey system to the initial model and the discretized measurements; comparing the forward model to the measured electromagnetic response to determine differences; adjusting the initial model to reduce the differences; and repeating generating a forward model, comparing the forward model to the measured electromagnetic response, and adjusting the initial model until the differences fall below a selected threshold.
    • 用于对水体下面的地层中的导电率分布进行建模的方法包括用电磁测量系统测量地层的电磁响应; 相对于水中的深度测量水导率,水介电常数和水温中的至少一个; 产生地层电导率分布的初始模型; 相对于至少一层的深度将水导电性,水介电常数和水温中的至少一种的测量离散化; 产生电磁勘探系统对初始模型和离散化测量的响应的正向模型; 将正向模型与测量的电磁响应进行比较,以确定差异; 调整初始模型以减少差异; 并且重复产生正向模型,将正向模型与所测量的电磁响应进行比较,以及调整初始模型,直到差值低于所选阈值。