I joined the Ocean University of China as an associate professfor starting from 2023. Before it, I was
a Postdoc at Princeton University in Jeroen Tromp's and Frederik J. Simons' Research
Groups (2020-2023). I received Ph.D. in Earth Science and Engineering from King Abdullah
University of Science and Technology (KAUST),
where I am advised by Gerard
My research interests lie in: (1) the application of 2D/3D elastic FWI to the land and marine surface seismic and VSP
data, (2) the application of machine learning to seismic data processing and migration, and (3)
3D surface wave inversion and migration. I have spent time at Los Alamos National Laboratory for
internship. I visited TOTAL for two weeks.
I'm interested in source encoded FWI, application of elastic FWI to the challenging seismic data,
application of machine learning to seismic data processing and migration,
3D surface wave inversion, seismic forward modeling
in frequency domain, superresolution imaging with surface waves, and natural migration of surface waves.
Representative papers are highlighted.
Solving Large-Scale Elastic Tomographic Problems with Source Encoding in the Laplace Domain
Zhaolun Liu, Jurgen Hoffmann, Frederik J. Simons, Jeroen Tromp, Etienne Bachmann, and Congyue Cui
SIAM Conference on Mathematical & Computational Issues in the Geosciences, 2023, (Oral Presentation)
Elastic Full Waveform Inversion (FWI) is a state-of-the-art seismic imaging
method that provides high-resolution subsurface images and yields
additional information compared to purely acoustic approaches. However, an
argument against using full-physics wave propagation is that it is
computationally expensive. The need for vast computing power to conduct 3-D
elastic FWI would seem to prevent its application to 3-D seismic
data. Crosstalk-free source encoding remedies the runaway computational
cost of full-physics FWI. It reduces the number of seismic sources by
forming encoded super-gathers. The main drawback of the source-encoded
FWI formulation arises from the difficulty of time windowing the modeled
data when inverting only one or a few sparsely sampled frequencies at
once. Yet, time windowing would allow for the selection of specific arrivals during the various stages of the inversion, which can effectively mitigate the nonlinearity of FWI. We propose the use of complex-valued frequencies through the Laplace transform for source-encoded FWI, in order to dampen arrivals starting at a given traveltime. In this talk, we will introduce the theory of Laplace-domain source-encoded FWI and demonstrate its effectiveness through numerical tests conducted on challenging seismic
datasets collected onshore and offshore.
Robust Multi-bin Wave Equation Dispersion Inversion Methods for High-resolution Seismic Imaging of Near-surface Geology
Zhaolun Liu, Yi Luo, and Ben Eppinger
Project Page IMAGE (SEG), 2023, (Oral Presentation)
Estimating the shallow wave speed model from land seismic data can be
challenging due to the complexity of near-surface structures.
When there is a significant velocity contrast or velocity reversal
in the near-surface, the early arrivals at large offsets will be
dominated by shingling events, while surface waves will dominate
late arrivals at near offsets. It can be almost impossible to pick
the first break of the shingling events, making traditional first-arrival
tomography methods prone to failure. In response to this challenge,
we propose a new, robust method that can invert shingling events and surface
waves in an accurate and reliable manner.
We demonstrate the effectiveness of our multi-bin WD algorithm by applying it
to invert shingling events from a complex layered
model. Next, we apply multi-bin WD to invert
surface waves for S-wave wave speed (VS). The results demonstrate the effectiveness of the multi-bin WD method.
3D Acoustic-Elastic Coupled Full Waveform Inversion of Marine VSP Data from Fenja Field, Norway
Zhaolun Liu, Jurgen Hoffmann, Frederik J. Simons and Jeroen Tromp
Project Page IMAGE (SEG), 2022, (Oral Presentation)
We apply the state-of-the-art three-dimensional (3D) acoustic-elastic coupled seismic modeling, migration, and inversion
techniques to deviated Rig Source Vertical Seismic Profile (RSVSP) data from the Fenja Field in Norway, to advance our understanding
of subsurface structure.
Elastic Full Waveform Inversion of VSP Data from a Complex Anticline in Northern Iraq
Zhaolun Liu, Jurgen Hoffmann, Frederik J. Simons and Jeroen Tromp
Project Page IMAGE (SEG), 2021, (Oral Presentation)
We demonstrate an application of isotropic elastic Full-Waveform Inversion
(FWI) to a field data set of Vertical Seismic Profiles (VSP) from a
structurally complex narrow anticline in Northern Iraq. Both RTM and LSRTM results show that
the shear wave speed (Vs) image has a higher resolution than the
compressional speed (Vp) image for the target structure, owing to the
presence of interpretable P-to-S converted waves.
The elastic LSRTM has improved the amplitude balancing and image resolution and mitigated some migration
artifacts compared to elastic RTM.
The seismic data with a relatively high signal-to-noise ratio are chosen for training to get the
learned basis functions. Then we use all (or a subset) of the basis functions to attenuate the random or
coherent noise in
the seismic data.
Irregular topography can cause strong scattering and defocusing of propagating surface
waves. Thus it is important to consider such effects when inverting surface waves for the
shallow S-velocity structures. Here, we present a 3D surface-wave dispersion inversion
method that takes into account the topographic effects modeled by a 3D spectral element
We recast the multilayered sparse inversion problem as a multilayered neural network problem.
Unlike standard least squares migration (LSM) which finds the optimal reflectivity image,
neural network least squares migration (NNLSM) finds both the optimal reflectivity image and the
SEG Annual Meeting, 2018, (Oral Presentation) Geophyscis, 2019
We extend the 2D wave-equation dispersion inversion (WD) method to 3D wave-equation inversion of
surface waves for the shear-velocity distribution.
Semi-stationary Supervirtual Interferometry of Reflections and Diving Waves
Kai Lu, Zhaolun Liu, and Xiaodan Ge
CSIM Annual Report, 2018 Geophyscis, 2020
we extend the application of SVI to far-offset reflections and diving waves by defining semi-stationary
Semi-stationary phases mean that the phase difference between adjacent traces in the common pair gather
(CPG) are very small, so that stacking the semi-stationary traces with techniques of limiting the
zone and phase shift compensation also enhances the SNR.
We have developed a methodology for detecting the pres-
ence of near-surface heterogeneities by naturally migrating
backscattered surface waves in controlled-source data.
This natural migration method does not require knowledge of the near-surface phase-velocity
distribution because it uses the recorded data to approximate the Green’s functions for migration.