P-wave velocity structures of the crust across the Southern Taiwan Strait imaged by using air-gun data recorded from ocean-bottom seismometers

Ocean-bottom seismometers (OBSs) were deployed at a shallow water depth (

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Bibliographic Details
Published in:Marine geophysical researches 2020-06, Vol.41 (2), Article 12
Main Authors: Wang, Tan K., Deng, Jia Ming, Wang, Jing, Cheng, Yu Hsuan, Xie, Zhi Zhao, Zhang, Yi Feng
Format: Article
Language:English
Subjects:
Cenozoic
Deformation
Earth and Environmental Science
Earth Sciences
Fault lines
Fault zones
Geological time
Geophysics/Geodesy
Graben
Hydrophones
Ocean bottom seismometers
Oceanography
Oceans
Offshore Engineering
Original Research Paper
Orogeny
P-waves
Rifting
Seismic wave velocities
Seismometers
Shallow water
Shoals
Straits
Travel time
Water depth
Wave velocity
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Description
Summary:Ocean-bottom seismometers (OBSs) were deployed at a shallow water depth (
ISSN:0025-3235
1573-0581
DOI:10.1007/s11001-020-09410-0