Dr. Wang graduated from the Beijing Med Univ, Beijing City, Beijing, China in 1986. He works in Hamilton Square, NJ and specializes in Internal Medicine and Diabetes. Dr. Wang is affiliated with Robert Wood Johnson University Hospital Hamilton, St Francis Medical Center and University Medical Center Of Princeton At Plainsboro.
Lankenau Medical Center Hematology/Medical Oncology Medical Program 100 E Lancaster Ave STE 4413, Wynnewood, PA 19096 (484)4763060 (phone), (484)4763577 (fax)
Education:
Medical School Sun Yat Sen Univ of Med Sci, Guangzhou, China (242 21 Pr 1/71) Graduated: 2000
Languages:
English
Description:
Dr. Wang graduated from the Sun Yat Sen Univ of Med Sci, Guangzhou, China (242 21 Pr 1/71) in 2000. She works in Wynnewood, PA and specializes in Hematology/Oncology.
Yonghe Sun - Cypress TX, US Yue Wang - Danville CA, US Tong Xu - Chengdu, CN Leonard Lin Zhang - Sugar Land TX, US
International Classification:
G01V 1/28
US Classification:
367 75
Abstract:
A method for determining values of anisotropic model parameters of a Tilted Transversely Isotropic (TTI) Earth model, the anisotropic parameters including P-wave velocity (Vp) along a tilted symmetry axis, the Thomsen anisotropy parameters δ and ε (or η=(ε−δ)/(1+2δ)) representative of variations of wave velocities as a function of wave propagation angle from the symmetry axis, the method including acquiring input data for a geological volume of interest; determining a theoretical relationship between the input data and the anisotropic model parameters; and calculating the values of the anisotropic model parameters at each of a plurality of subsurface locations in the geological volume of interest based on the theoretical relationships and the input data using workflows involving iterative or sequential combinations of processes including input data preprocessing, conventional tomographic inversion, three dimensional tomographic inversion based on a tilted transversely isotropic model, and three dimensional pre-stack depth migration using a tilted transversely isotropic model.
System And Method For Seismic Beam Formation That Accounts For Equipment Misalignment
Norman Ross Hill - Houston TX, US Yue Wang - Danville CA, US
International Classification:
G01V 1/28
US Classification:
367 53
Abstract:
Seismic data representing the propagation of seismic energy through a geologic volume of interest is processed. The seismic energy propagates through the geologic volume of interest from one or more source locations at or near the geologic volume of interest to one or more detector locations at or near the geologic volume of interest. In processing the seismic data, the seismic energy is modeled as beams (e.g., Gaussian beams). The processing performed (i) corrects for misalignment of the one or more source locations and/or the one or more detector locations with a regular, predetermined mesh, and (ii) steers the seismic data based on the modeled beams.
Method And System For Computational Acceleration Of Seismic Data Processing
A computer-implemented method and a system for computational acceleration of seismic data processing are described. The method includes defining a specific non-uniform memory access (NUMA) scheduling for a plurality of cores in a processor according to data to be processed; and running two or more threads through each of the plurality of cores.
Multiple Anisotropic Parameter Inversion For A Tti Earth Model Using Well Data
Yonghe Sun - Cypress TX, US Yue Wang - Danville CA, US Tong Xu - Cheng Du, CN Leonard Lin Zhang - Sugar Land TX, US
International Classification:
G06F 19/00
US Classification:
702 18
Abstract:
A method for determining values of anisotropic model parameters of a Tilted Transversely Isotropic (TTI) Earth model, the method including obtaining an initial TTI earth model that substantially flattens common-imaging-point gathers and substantially ties seismic data to well data; inputting checkshot data and/or VSP data to determine updated values of Vpnear the well locations; determining an incremental improvement Δδ; extrapolating the relative change Δδ from near-well locations to the entire three dimensional TTI earth model; determining updated values of Vp=Vp(1−Δδ); inputting near-to-mid-offset/angle and mid-to-far-offset/angle residual moveout information; and providing updated values of δ and η.
Linbin Zhang - Danville CA, US Wei Liu - San Ramon CA, US Yue Wang - Sugar Land TX, US Guojian Shan - San Ramon CA, US
Assignee:
Chevron U.S.A. Inc. - San Ramon CA
International Classification:
G06F 19/00
US Classification:
702 14
Abstract:
Various embodiments provide a system and a shot illumination compensation method implemented on a computer system for imaging a subsurface formation. The method includes receiving, by the computer system, seismic data produced by an acoustic energy source and reflected by the subsurface formation; and generating, by the computer system, an image of the subsurface formation based on the seismic data and a spatially varying damping parameter.
System And Method For Seismic Imaging Of Complex Subsurface Volumes
- San Ramon CA, US Yue WANG - Sugar Land TX, US Siwei LI - Houston TX, US
International Classification:
G01V 1/34 G01V 1/36 G01V 1/28 G01V 1/30
Abstract:
A method is described for seismic imaging including generating extended image gathers by extended reverse time migration of a seismic dataset using an earth model; processing the extended image gathers to generate processed image gathers; performing extended modeling based on the processed image gathers to generate a modeled seismic dataset; enhancing the processed image gathers to generate an enhanced image; performing extended modeling based on the enhanced image gathers to generate a modeled enhanced dataset; differencing the modeled enhanced dataset and the modeled seismic dataset to determine a data residual; inverting the data residual to generate a model residual; updating the earth model based on the model residual to create an updated earth model; performing seismic imaging of the seismic dataset using the updated earth model to create an improved seismic image. The method may be executed by a computer system.
System And Method For Dip-Guided Seismic Image Stacking
- San Ramon CA, US Guojian Shan - Sugar Land TX, US Yue Wang - Sugar Land TX, US Craig Alan Barker - Sugar Land TX, US
International Classification:
G01V 1/30 G01V 1/36
Abstract:
A method is described for seismic imaging of the subsurface using dip-guided optimized stacking. The method computes weighting functions for a plurality of single-shot migrated images, unstacked seismic images, or partially stacked seismic images based on a slant stack performed using an input dip dataset; applying the plurality of weighting functions to the plurality of single-shot migrated images, unstacked seismic images, or partially stacked seismic images, or a plurality of dip-filtered images to create a plurality of weighted images; and summing the plurality of weighted images into a stacked seismic image. The method may be executed by a computer system.
System And Method For Velocity Analysis In The Presence Of Critical Reflections
Yonghe J. Sun - Cypress TX, US Yue Wang - Sugar Land TX, US Jianlei Liu - Katy TX, US Leonard Lin Zhang - Sugar Land TX, US
Assignee:
CHEVRON U.S.A. INC. - San Ramon CA
International Classification:
G01V 1/30 G01V 1/36
Abstract:
A method is described for processing residual moveout in seismic image data gathers representing critical reflections. The method includes receiving seismic image data arranged as a function of an angle or offset parameter including a high-velocity-contrast event with post-critical. The method also includes applying a wavelet de-stretch filter to the seismic data to correct wavelet stretching. The method also includes applying a fan-filter to remove coherent noise in the one or more post-critical traces; picking residual moveout of the high-velocity-contrast event; adjacent-trace differencing to detect the impact of phase change at critical reflections in residual moveouts, and applying a median-filter to the residual moveout to reduce the impact of phase change of the high-velocity-contrast event in the one or more post-critical traces. The median-filtered and reconstructed residual moveout is used for improving a velocity model used for generating the seismic image gathers.