Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Zuoyong Lv"'
Autor:
Jiajia Song, Shuaijun Wang, Yonghong Duan, Xiuwei Ye, Zuoyong Lv, Liang Wang, Baofeng Liu, Xianghui Song, Guoliang Cheng, Mingming Ruan
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
This study presents an interpretation of a deep seismic sounding (DSS) profile that carried out along the Cathaysia Block in southeast china, aiming to explore the crustal velocity structure. Data used in the survey were obtained from three controlle
Externí odkaz:
https://doaj.org/article/292b82bc659b46d9aa99a5ca00bb594b
Autor:
Weilai Wang, Zuoyong Lv, Long Zhang, Guangdong Earthquake Agency, Guangzhou , China, Lihua Fang
Publikováno v:
Earthquake Science. 33:72-81
The Pear River Estuary (PRE) area is located in the northern margin of South China Sea (SCS), which is a typical rifted passive continental margin between the South China Block and SCS Basin. The Littoral Fault Zone (LFZ) crossing the PRE is an impor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad02670999bf64e0d94a5433e5f31e29
https://doi.org/10.5194/egusphere-egu2020-12225
https://doi.org/10.5194/egusphere-egu2020-12225
To find out the crustal structure and tectonic attribute of the Pearl river delta and offshore area(PRD), in 2015, the Guangdong Earthquake Agency collaboration with the other unit carried out a three-dimensional joint onshore-offshore seismic detect
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7eab01ff40cb00f29170d0623c99f1d
https://doi.org/10.5194/egusphere-egu2020-2343
https://doi.org/10.5194/egusphere-egu2020-2343
Autor:
Xiuwei Ye, Xuelin Qiu, Haibo Huang, Xiaona Wang, Liwei Wang, Sun Wang, Jinshui Lv, Zuoyong Lv
Publikováno v:
International Geology Review. 62:1057-1069
The land-sea transition zone in the northern South China Sea (SCS) records important information from the continental rifting to the seafloor spreading. The crustal structure is the key to explore the deep tectonic environment and the evolution of th