ON-SITE EARTHQUAKE EARLY WARNING SYSTEM AND METHOD

    公开(公告)号:US20240248221A1

    公开(公告)日:2024-07-25

    申请号:US18156582

    申请日:2023-01-19

    申请人: P-Waver Inc.

    IPC分类号: G01V1/00 G01V1/28

    CPC分类号: G01V1/008 G01V1/284

    摘要: An on-site earthquake early warning method is disclosed. The method includes the following steps: receiving a first signal generated in response to a first vibration event and a second signal generated in response to a second vibration event; determining whether an earthquake event exists according to the first and the second signals; predicting a real-time seismic shear wave prediction characteristic value according to the first signal; and sending the real-time seismic shear wave prediction characteristic value when it is determined that the earthquake event exists.

    Subsurface wave slowness prediction system

    公开(公告)号:US11719840B2

    公开(公告)日:2023-08-08

    申请号:US16499955

    申请日:2018-12-28

    IPC分类号: G01V1/50 G01V1/28 G01V1/30

    摘要: An apparatus includes a mechanical wave source; a set of mechanical wave sensors in a borehole to provide subsurface wave measurements based on formation waves from the mechanical wave source, and a processor. The apparatus also includes a machine-readable medium having program code to acquire the subsurface wave measurements, select a first set of tool wave measurements based on the subsurface wave measurements, and generate a set of filtered subsurface wave measurements by filtering the subsurface wave measurements based on the first set of tool wave measurements. The program code also includes instructions to generate a time-domain semblance map based on the set of filtered subsurface wave measurements, wherein the time-domain semblance map includes an initial set of compression wave peaks, determine a selected qualified compression wave peak based on a semblance value in the time-domain semblance map, and determine a compression wave slowness based on the selected qualified compression wave peak.

    Omnidirectional Vector Seismic Data Processing Method And Apparatus, Computer-Readable Storage Medium And Device

    公开(公告)号:US20180246238A1

    公开(公告)日:2018-08-30

    申请号:US15965503

    申请日:2018-04-27

    IPC分类号: G01V1/28 G01V1/30 G01V1/18

    摘要: The invention discloses an omnidirectional vector seismic data processing method and apparatus, a computer readable storage medium and a device, applied to an omnidirectional vector geophone. Wherein the method comprises: collecting omnidirectional vector seismic data of the omnidirectional vector geophone, and performing a pre-processing operation on the omnidirectional vector seismic data; performing pressure and shear waves separation operation on the omnidirectional vector seismic data after the data is subject to the pre-processing operation, to obtain pressure wave data and shear wave data; sequentially performing space vector calculation, a wave field recovery operation and an imaging operation on the pressure wave data and the shear wave data, and then performing modeling to obtain a pressure wave velocity model and a shear wave velocity model. The invention solves the problem of the existing seismic exploration technology that cannot measure and process divergence data and curl data of seismic wave field, so as to improve construction, lithology, fluid exploration accuracy and reliability and promote seismic exploration to be developed from structural exploration to lithology exploration and fluid exploration.

    JOINT INVERSION OF COMPRESSIONAL AND SHEAR SEISMIC DATA IN NATIVE TIME DOMAINS

    公开(公告)号:US20170322331A1

    公开(公告)日:2017-11-09

    申请号:US15329458

    申请日:2015-08-18

    申请人: CGG SERVICES SAS

    发明人: Benjamin ROURE

    IPC分类号: G01V1/28 G01V1/30

    CPC分类号: G01V1/284 G01V1/301 G01V1/305

    摘要: PP and PS seismic data are jointly inverted in a stratigraphic grid, using different time axes for PP and PS reflections. A ratio of PP and of PS waves'travel times inside a same layer cell maintained to be a function of a ratio of a P-wave propagation velocity and of an S-wave propagation velocity therein. Since PP and PS seismic amplitudes and travel times are due to elastic properties of the same structure, they can be inverted at the same time to provide better estimates of these elastic properties.