Welcome to Weihong
Fei's Homepage
Weihong Fei
Center for Lithospheric Studies, The
Phone :
214-683-6293 (cell); 972-437-5908 (home)
Fax
: 972-883-2829
E_mail : weihong.fei@student.utdallas.edu
Research
Interest
Seismic
velocity analysis, seismic migration, seismic data processing
Working
Experience
5/2005-8/2005 internship in BGP,
5/2003-8/2003 internship in Total , 3-D prestack parsimonious migration in CDP domain.
1/2003-5/2003 internship in Total, parallization and optimization of parsimonious
migration.
7/2000-8/2001 worked for Beijing City
Geological Survey Technical Institute as a geophysical engineer.
Education
8/2001-now Pursuing Ph.D. degree in
exploration geophysics under the supervision of George A. McMechan. Expected August, 2005
Research
topics: velocity
analysis, seismic migration, data processing
Awards:
First place of the ‘Best student paper’ in 2004 UTD
consortium meeting
Second place of the ‘Best student
paper’ in 2005 UTD consortium meeting
Second
prize in SEG/AAPG student expo 2004
9/97-7/2000 Institute of
Degree:
MS
Research
topics: Sedimentology and basin modeling
Awards:
Scholarship for excellent students in
Excellent
Thesis
9/93-7/97
Geology Department,
Degree:
BS
Major:
Geology
Awards:
Scholarship for 4 consecutive years
Publications
1. 3-D fast reflectorless tomographic seismic migration velocity analysis
2. Fast model-based migration velocity analysis
and reflector shape estimation (Geophysics,
v70, 2005) (This paper is selected as
one of the bright spots of issues 2, v70, see The Leading
Edge, 2005, v24, p394)
3. Reflectorless tomographic seismic migration velocity analysis (submitted
to Geophysics).
4. Fei Weihong, Li Zhong,
Wang Shenglang. The quartz overgrowths and their
reflection to the fluid flows in Qiaokou-Baimiao
region, Dongpu Depression. Scientia Geologica Sinica
(2001,8:312-321).
5. Li Zhong and Fei Weihong. 1999. Evolution and physical properties of sandstone
reservoirs: constraints on high-pressure tight
gas deposits in Dongpu Depression,
3-D
Velocity Analysis Result

Figure 1. Comparison
between the correct velocity model (top) and the estimated velocity
model
(bottom), the starting velocity model for tomography is constant.


Figure 2. The comparison
between the migration images using the estimated
3-D velocity
model and true velocity model