Zhouchuan Huang
YOU?
Author Swipe
View article: Correction: Investigating acid mine drainage in complex topography areas via semi-airborne and surface geophysical surveys: a case study in Fujian, China
Correction: Investigating acid mine drainage in complex topography areas via semi-airborne and surface geophysical surveys: a case study in Fujian, China Open
View article: Accurate detection of hidden faults in Xianlin area, Nanjing (China) based on a dense, short-period seismic array
Accurate detection of hidden faults in Xianlin area, Nanjing (China) based on a dense, short-period seismic array Open
SUMMARY High-resolution detection of hidden geological faults is vital for city planning, earthquake disaster prevention and large-scale engineering construction. This study deployed 229 short-period seismometers across a 10×30 km region w…
View article: Seismic Anisotropy Variations in the Eastern Mediterranean Sea Region Revealed by Splitting Intensity Tomography: Implications on Mantle Dynamics
Seismic Anisotropy Variations in the Eastern Mediterranean Sea Region Revealed by Splitting Intensity Tomography: Implications on Mantle Dynamics Open
Reliable knowledge of seismic anisotropy in the mantle can provide invaluable insights into complex tectonics and geodynamics in Anatolia controlled by intricate plate interactions across the region. However, the 3D variations in seismic a…
View article: The return of stagnant slab recorded by intraplate volcanism
The return of stagnant slab recorded by intraplate volcanism Open
Subducted plates often stagnate in the mantle transition zone (MTZ), and the fate of the stagnant slabs is still debatable. They may sink into the lower mantle, or remain partially trapped in the MTZ, but it is uncertain whether they can r…
View article: An iterative weighted least-square fitting method for crustal anisotropy using receiver functions
An iterative weighted least-square fitting method for crustal anisotropy using receiver functions Open
SUMMARY The harmonic variation of the P-to-S converted phases (i.e. Pms) observed from receiver functions (RFs) includes information on crustal azimuthal anisotropy. However, this harmonic analysis is easily influenced by low-quality RF tr…
View article: A review of geophysical studies on the Mongolian Plateau
A review of geophysical studies on the Mongolian Plateau Open
The Mongolian Plateau in Central Asia is an intracontinental tectonic system far from active plate boundaries. Despite its distance from these boundaries, the plateau is characterized by intense crustal deformation accompanied by voluminou…
View article: Upper-mantle velocity structures and anisotropy under the Mongol-Baikal region
Upper-mantle velocity structures and anisotropy under the Mongol-Baikal region Open
The Mongol-Baikal region is located in the western segment of the Central Asian Orogenic Belt. This area experienced multiple periods of extensive compression starting from the Proterozoic. In the Cenozoic, the study region was modified by…
View article: Gssfnet: Graph-Based Spectral-Spatial Fusion Network for Hyperspectral Image Classification
Gssfnet: Graph-Based Spectral-Spatial Fusion Network for Hyperspectral Image Classification Open
View article: Multi-scale anisotropy in NE China: Evidence for localized mantle upwelling
Multi-scale anisotropy in NE China: Evidence for localized mantle upwelling Open
It is commonly proposed that the subduction of the Pacific plate has been responsible for widespread Holocene intraplate volcanism across NE China and the Korean Peninsula. Yet, how this process drives volcanism and even if it plays a crit…
View article: Reproducing complex anisotropy patterns at subduction zones from splitting intensity analysis and anisotropy tomography
Reproducing complex anisotropy patterns at subduction zones from splitting intensity analysis and anisotropy tomography Open
SUMMARY Measurements of seismic anisotropy provide a lot of information on the deformation and structure as well as flows of the Earth's interior, in particular of the upper mantle. Even though the strong and heterogeneous seismic anisotro…
View article: Seismic anisotropy and geodynamics of the East Japan subduction zone
Seismic anisotropy and geodynamics of the East Japan subduction zone Open
Seismic anisotropy in the East Japan arc has been extensively investigated by conducting shear-wave splitting measurements, receiver-function analyses, and tomographic inversions of body-wave travel times and surface-wave dispersion data, …
View article: High-resolution imaging of the deep structure of Italy through SKS anisotropy tomography
High-resolution imaging of the deep structure of Italy through SKS anisotropy tomography Open
Seismic anisotropy is a fundamental key to gain knowledge of the mantle dynamics and structure. The image of seismic anisotropy over the upper mantle can be obtained with several methods, including surface waves and SKS splitting measureme…
View article: Novel Application of Receiver Function Analyses Dependent on Splitting Measurement: Crustal Anisotropy along the NAFZ
Novel Application of Receiver Function Analyses Dependent on Splitting Measurement: Crustal Anisotropy along the NAFZ Open
Crustal scale deformation along the fault zone and dipping Moho structures can be constrained by azimuthal seismic anisotropy. Reliable knowledge of the geometry of fault and its vertical extent in the crust and uppermost mantle that often…
View article: Stepwise Lithospheric Delamination Leads to Pulsed Cenozoic Uplifts of Central Tien Shan
Stepwise Lithospheric Delamination Leads to Pulsed Cenozoic Uplifts of Central Tien Shan Open
The Tien Shan provides an ideal site to study mechanism of intracontinental orogeny due to distant effect of Indo-Asian collision. We investigate lithospheric structures, in particular the lithosphere-asthenosphere boundary (LAB), of Centr…
View article: Structural Heterogeneity of the Alaska‐Aleutian Forearc: Implications for Interplate Coupling and Seismogenic Behaviors
Structural Heterogeneity of the Alaska‐Aleutian Forearc: Implications for Interplate Coupling and Seismogenic Behaviors Open
We determine high‐resolution 3‐D seismic images ( Vp , Vs , and Vp / Vs ) of the Alaska‐Aleutian forearc region, which are used to further estimate the serpentinization volume fraction of the subducting Pacific slab. Our results show that …
View article: Seismotectonics of Mongolia and Baikal Rift Zone Controlled by Lithospheric Structures
Seismotectonics of Mongolia and Baikal Rift Zone Controlled by Lithospheric Structures Open
Active tectonics are developing in Mongolia and the Baikal rift zone, where large crustal earthquakes (Mw ≥ 6.0) occur frequently. To clarify the mechanism of these earthquakes, we determine a high‐resolution 3‐D P ‐wave velocity model of …
View article: Crustal and Uppermost Mantle Heterogeneities Across the Ailaoshan Red River Shear Zone, SE Tibet: Implications for Cenozoic Magmatic Activity
Crustal and Uppermost Mantle Heterogeneities Across the Ailaoshan Red River Shear Zone, SE Tibet: Implications for Cenozoic Magmatic Activity Open
The Ailaoshan Red River shear zone (ARSZ) was formed in the Mesozoic as a suture zone between the Indochina block and the Yangtze craton. Since the Cenozoic, block extrusion due to the Indo‐Asian collision has reactivated the fault zone an…
View article: D″ anisotropy inverted from shear wave splitting intensity
D″ anisotropy inverted from shear wave splitting intensity Open
The D″ layer, located at the bottom of the mantle, is an active thermochemical boundary layer. The upwelling of mantle plumes, as well as possible plate subduction in the D″ layer, could lead to large-scale material transformation and mine…
View article: High-resolution imaging of subduction zones through SKS splitting intensity tomography: first results from test on numerically modelled complex settings
High-resolution imaging of subduction zones through SKS splitting intensity tomography: first results from test on numerically modelled complex settings Open
<p>Measurements of seismic anisotropy provide a lot of information on the deformation and structure of the upper mantle, as well as flow in the Earth’s interior. High-resolution seismic anisotropy in the upper mantle can be…
View article: Mantle dynamics in the SE Tibetan Plateau revealed by teleseismic shear-wave splitting analysis
Mantle dynamics in the SE Tibetan Plateau revealed by teleseismic shear-wave splitting analysis Open
View article: Crustal and Uppermost Mantle Isotropic and Anisotropic P-wave Velocity Variations Beneath Turkey&#160;
Crustal and Uppermost Mantle Isotropic and Anisotropic P-wave Velocity Variations Beneath Turkey  Open
<p>Turkey has been undergoing compressional and extensional tectonics that greatly influences the major surface features following northward plate convergences since the Miocene. Despite increasing efforts in last few decades aiming …
View article: Seismic structure and subduction dynamics of the western Japan arc
Seismic structure and subduction dynamics of the western Japan arc Open
Recent findings on the seismic structure and subduction dynamics of the western Japan arc are reviewed. High-resolution seismic velocity and attenuation tomography has imaged the subducting Pacific and Philippine Sea (PHS) slabs clearly. L…
View article: Isotropic and Anisotropic <i>P</i> Wave Velocity Structures of the Crust and Uppermost Mantle Beneath Turkey
Isotropic and Anisotropic <i>P</i> Wave Velocity Structures of the Crust and Uppermost Mantle Beneath Turkey Open
Compressional and extensional tectonics following northward plate convergences since the Miocene have formed the major surface features in Turkey, such as faulting and orogeny. Despite increasing efforts in last few decades aiming to eluci…
View article: Sharp Lateral Moho Variations Across the SE Tibetan Margin and Their Implications for Plateau Growth
Sharp Lateral Moho Variations Across the SE Tibetan Margin and Their Implications for Plateau Growth Open
The tectonic uplift of the Tibetan Plateau is a focus in the geosciences. Middle‐lower crustal flow is a popular model to interpret the geodynamic mechanism on the margin of the Tibetan Plateau. The model predicts different surface and Moh…
View article: Structural Heterogeneity in Source Zones of the 2018 Anchorage Intraslab Earthquake and the 1964 Alaska Megathrust Earthquake
Structural Heterogeneity in Source Zones of the 2018 Anchorage Intraslab Earthquake and the 1964 Alaska Megathrust Earthquake Open
Structural heterogeneities in subduction zones can affect slip behaviors of the megathrust faults and the generation of intraslab earthquakes. In this work we study the 3‐D seismic structures (Vp, Vs, and Poisson's ratio) in and around the…
View article: Geochemical analysis of Lake Baikal sediments: review of the results of the Sino-Russian joint expedition at Lake Baikal as a scientific training project
Geochemical analysis of Lake Baikal sediments: review of the results of the Sino-Russian joint expedition at Lake Baikal as a scientific training project Open
The article presents the materials that have been collected, processed and prepared for publication by the students participating in the international Sino-Russian scientific educational field expedition "Baikal as the world's pearl, 2019"…
View article: <i>P</i> and <i>S</i> Wave Tomography Beneath the SE Tibetan Plateau: Evidence for Lithospheric Delamination
<i>P</i> and <i>S</i> Wave Tomography Beneath the SE Tibetan Plateau: Evidence for Lithospheric Delamination Open
The SE Tibetan Plateau is located between the eastern Himalayan syntaxis and the stable Yangtze craton; its tectonic evolution is important for understanding the plateau expansion. However, interactions between the plateau and its adjacent…
View article: Structural Heterogeneity and Anisotropy in the Source Zone of the 2018 Eastern Iburi Earthquake in Hokkaido, Japan
Structural Heterogeneity and Anisotropy in the Source Zone of the 2018 Eastern Iburi Earthquake in Hokkaido, Japan Open
We investigate 3‐D seismic structures ( Vp , Vs , and Poisson's ratio) and Vp azimuthal anisotropy in the source area of the 2018 Eastern Iburi earthquake (M 6.7) in Hokkaido, Japan. Its mainshock occurred at the edge of a high‐Vp (2–4%) s…
View article: A method of simultaneously measuring crustal azimuthal anisotropy and Moho geometry based on receiver functions
A method of simultaneously measuring crustal azimuthal anisotropy and Moho geometry based on receiver functions Open
View article: Insight into the NE Tibetan Plateau expansion from crustal and upper mantle anisotropy revealed by shear‐wave splitting
Insight into the NE Tibetan Plateau expansion from crustal and upper mantle anisotropy revealed by shear‐wave splitting Open