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Inversion of Shallow Velocity Structure in Northern Tangshan Using First Arrival Traveltime from Deep Reflection Profile
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Jia JIA1, Fuyun WANG1, Qiaoxia LIU1, *, Yonghong DUAN1, Zhenyu FAN1, Hongwei WANG1, Zhanyong GAO1
Journal of Geodesy and Geodynamics | 2025, 45(8) : 834 - 839
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Journal of Geodesy and Geodynamics | 2025, 45(8): 834-839
Inversion of Shallow Velocity Structure in Northern Tangshan Using First Arrival Traveltime from Deep Reflection Profile
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Jia JIA1, Fuyun WANG1, Qiaoxia LIU1, *, Yonghong DUAN1, Zhenyu FAN1, Hongwei WANG1, Zhanyong GAO1
Affiliations
  • 1 Geophysical Exploration Center, CEA, 75 Wenhua Road, Zhengzhou 450002, China
  • JIA Jia, engineer, majors in seismic tomography imaging and fault zone detection, E-mail:

About Author:

JIA Jia, engineer, majors in seismic tomography imaging and fault zone detection, E-mail:

Published: 2025-08-15 doi: 10.14075/j.jgg.2024.09.428
Outline
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The first arrival travel times of a deep reflection profile, approximately 30 km long, implemented along the northwest-southeast direction across the northern segment of the Tangshan fault in 2023 were inverted to obtain a detailed shallow velocity structure profile in the northern part of Tangshan. The velocity structure profile reveals that from 2.5 to 8.5 km along the survey line, the Cenozoic Era sediments are about 150 m thick and relatively uniform. The Fengtai-Yejituo fault is hidden at the survey line coordinate of 3.5 km, trending northwest, and F2-1 fault is hidden at 8.5 km, trending southeast; there is a hidden bulge between these two faults that is low in the northwest and high in the southeast. From 8.5 to 15.2 km along the survey line, the Cenozoic Era sediments gradually thicken from northwest to southeast, with a maximum thickness of about 250 m, indicating that the Jinggezhuang depression is a gull-shaped Cenozoic fault depression. The Douhe fault is exposed at 15.2 km, trending northwest. From 15.2 to 24 km along the survey line, it is the Tangshan uplift, with only local areas having very thin Cenozoic Era sediments, and the P-wave velocity at the same depth is much higher than on both sides; there is a nearly vertical low-velocity zone under Weishan, extending at least 600 m downward, which is speculated to be the fault zone of the Tangshan-Weishan-Changshan south slope fault belt. From the survey line coordinate of 24 km to the end of the survey line, it is the northwestern part of the Kaiping depression, showing a regular basin edge morphology, with Cenozoic Era sediments of about 130 m. The Douhe fault and the Tangshan-Weishan-Changshan fault are active faults of the Quaternary.

northern Tangshan  /  first arrival travel time tomography  /  shallow velocity structure  /  fault activity  /  geological structure
贾佳, 王夫运, 刘巧霞, 段永红, 范振宇, 王宏伟, 高占永. 利用深反射剖面初至波走时反演唐山市北部浅层速度结构. 大地测量与地球动力学, 2025 , 45 (8) : 834 -839 . DOI: 10.14075/j.jgg.2024.09.428
Jia JIA, Fuyun WANG, Qiaoxia LIU, Yonghong DUAN, Zhenyu FAN, Hongwei WANG, Zhanyong GAO. Inversion of Shallow Velocity Structure in Northern Tangshan Using First Arrival Traveltime from Deep Reflection Profile[J]. Journal of Geodesy and Geodynamics, 2025 , 45 (8) : 834 -839 . DOI: 10.14075/j.jgg.2024.09.428
  • National Natural Science Foundation of China(42074070)
  • National Natural Science Foundation of China(42374073)
  • Youth Fund of Geophysical Exploration Center, CEA(YFGEC2022005)
  • National Key Research and Development Program of China(2017YFC1500202)
Year 2025 volume 45 Issue 8
28
11
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Article Info
doi: 10.14075/j.jgg.2024.09.428
  • Receive Date:2024-09-09
  • Online Date:2026-10-29
  • Published:2025-08-15
Article Data
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History
  • Received:2024-09-09
Funding
National Natural Science Foundation of China(42074070)
National Natural Science Foundation of China(42374073)
Youth Fund of Geophysical Exploration Center, CEA(YFGEC2022005)
National Key Research and Development Program of China(2017YFC1500202)
Affiliations
    1 Geophysical Exploration Center, CEA, 75 Wenhua Road, Zhengzhou 450002, China
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表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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