financially supported by the National Key R&D Program of China(2018YFA0702504);the National Natural Science Foundation of China(42174152);the Strategic Cooperation Technology Projects of China National Petroleum Corporation(CNPC)and China University of Petroleum-Beijing(CUPB)(ZLZX2020-03);the R&D Department of China National Petroleum Corporation(2022DQ0604-01)。
The picking efficiency of seismic first breaks(FBs)has been greatly accelerated by deep learning(DL)technology.However,the picking accuracy and efficiency of DL methods still face huge challenges in low signal-to-nois...
supported by National Natural Science Foundation of China (42074157);the National Key Research and Development Program of China (2018YFC0310104);the Strategic Priority Research Program of the Chinese Academy of Science(XDA14010203)。
Reflection-based inversion that aims to reconstruct the low-to-intermediate wavenumbers of the subsurface model, can be a complementary to refraction-data-driven full-waveform inversion(FWI), especially for the deep t...
funded by the National Key R&D Program of China (No. 2020YFA0710600);National Science Foundation of China (No. 41374098);the Special Fund of the Institute of Geophysics,China Earthquake Administration (No. DQJB19B40)
The Tilted tilted transversely isotropic(TTI)media,a kind of anisotropic medium,widely exists within the earth.For faster calculation of travel times in the TTI anisotropic media,we modifi ed a minimum traveltime tree...
Supported by projects of National Natural Science Foundation of China(No.41804100);Fundamental Research Funds for the Central Universities(No.2682018CX36);China Postdoctoral Science Foundation(No.2020T130080);China Postdoctoral Science Foundation(No.2018M640910).
Geophysical exploration methods are important tools for landslide disaster assessment,landslide treatment scheme design,and landslide prevention engineering.Seismic exploration,as an important geophysical exploration ...
This research is jointly sponsored by National Natural Science Foundation of China(Grant No.U1901602);Shenzhen Key Laboratory of Deep Offshore Oil and Gas Exploration Technology(Grant No.ZDSYS20190902093007855);Shenzhen Science and Technology Program(KQTD20170810111725321);This study is also sponsored by the China Earthquake Science Experiment Project of China Earthquake Administration(Grant No.2018CSES0101).
Accurate calculations of travel times and raypaths of reflection waves are important for reflection travel time tomography.The multistage shortest path method(MSPM)and multistage fast marching method(MFMM)have been wi...
supported by the National Natural Science Foundation of China(No.41874167);the National Science and Technology Major Project of China(No.2017YFB0202904);the National Natural Science Foundation of China(No.41904130)。
Marchenko imaging obtains the subsurface reflectors using one-way Green’s functions,which are retrieved by solving the Marchenko equation.This method generates an image that is free of spurious artifacts due to inter...
Supported by projects of the Natural Science Foundation of China(No.41804100);the China Postdoctoral Science Foundation(No.2018M640910);the Fundamental Research Funds for the Central Universities(No.2682018CX36)
Kirchhoff beam migration is a beam migration method, which focuses on rapid imaging of geological structures. Although this imaging method ignores the amplitude information in the calculation process, it can calculate...
financial support for this work contributed by the National Key Research and Development Program of China(grant nos.2016YFC0600302,2016YFC0600101 and 2016YFC0600201);the National Natural Science Foundation of China(grants 41604075,41430213,41574092 and 41474068)
Irregular surface flattening,which is based on a boundary conforming grid and the transformation between curvilinear and Cartesian coordinate systems,is a mathematical method that can elegantly handle irregular surfac...
supported in part by National Basic Research Program of China (No. 2014CB845900);Hubei Provincial Natural Science Foundation of China (No. 2014CFA005)
Finite difference methods have been widely employed in solving the eikonal equation so as to calculate traveltime of seismic phase. Most previous studies used regular orthogonal grid. However, much denser grid is requ...
funded by the Spark Program of Earthquake Sciences (XH13012);China Earthquake Administration,and a Key Scientific and Technological Program of Earthquake Administration of Fujian Province (201202)
The paper collects the records by the Fujian Digital Seismic Network of 40 shallow earthquakes in Taiwan with M_S≥5.0 from 1999 to 2013,analyzes the seismic phase(Pn,Sn phase)characteristics and travel-time rules,det...