Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Wen-Nan Wu"'
Publikováno v:
Geoscience Letters, Vol 11, Iss 1, Pp 1-14 (2024)
Abstract Accurately imaging seismogenic structures is crucial for seismic hazard assessment. This is especially important around the deformation front (DF) region off SW Taiwan, where seismic potential is high but the fault structure and seismic acti
Externí odkaz:
https://doaj.org/article/c80f8471ccc848ae8e6baca7e03e3d3f
Publikováno v:
Geoscience Letters, Vol 10, Iss 1, Pp 1-13 (2023)
Abstract The Ryukyu trench-arc-back arc system is part of the subduction margins of the Philippine Sea plate. Previous studies have indicated that several geophysical and geological characteristics reveal significant variations (including convergent
Externí odkaz:
https://doaj.org/article/178218dbbbb6430d984bf3e18e770654
Autor:
Jing-Yi Lin, Wen-Nan Wu, Chih-Chieh Su, Ching-Hui Tsai, Hsu-Hsiao Sun, Yen-Fu Chen, Shao-Jinn Chin, Yi-Chin Lin
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 30, Iss 5, Pp 621-631 (2019)
Located to the south of East China Sea, the Southern Okinawa Trough (SOT) is a back-arc basin, which belongs to the Ryukyu subduction system. SOT is characterized by an active normal faulting system and numerous volcanic outcrops, which could have ma
Externí odkaz:
https://doaj.org/article/812b2f6b72c3471292d4c8d55406ca24
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 30, Iss 5, Pp 613-619 (2019)
The tectonic stress in the Ilan Plain (IP), NE Taiwan region is complex. Because the Philippine Sea plate converges and subducts beneath the Eurasian plate, and the Okinawa trough is rifting westward. We adopt the focal mechanisms collection during t
Externí odkaz:
https://doaj.org/article/636a8331614d40ffb36b692d180edce1
Autor:
Jing-Yi Lin, Yen-Fu Chen, Chih-Chieh Su, Shao-Jinn Chin, Win-Bin Cheng, Wen-Nan Wu, Chin-Wei Liang, Hsin-Sung Hsieh, Shu-Kun Hsu, Yi-Chin Lin
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 29, Iss 1, Pp 51-63 (2018)
Widely distributed Bottom-Simulating Reflectors (BSRs) have been observed in the area offshore of southwestern Taiwan where the active accretionary complex meets with the passive China continental margin. In order to clarify the link between seismic
Externí odkaz:
https://doaj.org/article/ba4777807d36430f82f44145afbe2714
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 26, Iss 6, p 619 (2015)
We undertook an investigation of the seismic behavior of large earthquake and estimated the crustal deformation state in the northern Philippine area in terms of the radial component of seismic moment tensors (Mrr) distribution. Based upon these two
Externí odkaz:
https://doaj.org/article/f40fc0df474c4648900a312596b07c36
Autor:
Wen-nan Wu, 吳文男
98
To understand the convergent characteristics of the westernmost plate boundary between the Philippine Sea plate and Eurasian plate, we have calculated the stress states of plate motion by focal mechanisms. Cataloged by the Harvard centroid mo
To understand the convergent characteristics of the westernmost plate boundary between the Philippine Sea plate and Eurasian plate, we have calculated the stress states of plate motion by focal mechanisms. Cataloged by the Harvard centroid mo
Externí odkaz:
http://ndltd.ncl.edu.tw/handle/97912507101973885934
Autor:
Wen Bin Doo, Hao Kuo-Chen, Hsueh Fen Wang, Yin Sheng Huang, Shiou Ya Wang, Wen Nan Wu, Chung Liang Lo
Publikováno v:
Terra Nova. 33:407-414
Autor:
Ching Hui Tsai, Hsu Hsiao Sun, Yi Chin Lin, Yen Fu Chen, Jing Yi Lin, Wen Nan Wu, Chih-Chieh Su, Shao Jinn Chin
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 30, Iss 5, Pp 621-631 (2019)
Located to the south of East China Sea, the Southern Okinawa Trough (SOT) is a back-arc basin, which belongs to the Ryukyu subduction system. SOT is characterized by an active normal faulting system and numerous volcanic outcrops, which could have ma
Autor:
Shu Kun Hsu, Yin Sheng Huang, Chung Liang Lo, Wen Nan Wu, Jing Yi Lin, Hsueh Fen Wang, Wen Bin Doo
Publikováno v:
Tectonophysics. 723:223-228
Understanding the strength of a plate coupling is critical for assessing potential seismic and tsunamic hazards in subduction zones. The interaction between an overriding plate and the associated subducting plate can be used to evaluate the strength