Zobrazeno 1 - 10
of 46
pro vyhledávání: '"Chung Liang Lo"'
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
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:
Wen-Bin Doo, Shu-Kun Hsu, Hsueh-Fen Wang, Yin-Sheng Huang, Ching-Hui Tsai, Chung-Liang Lo, Shiao-Shan Lin, Chin-Wei Liang, Yi-Jung Lin
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 30, Iss 5, Pp 675-683 (2019)
The Okinawa Trough (OT) is widely recognized as an area with extensive volcanism and hydrothermal activity. However, finding new hydrothermal vent sites in this region remains a technical challenge due to their small sizes. A deep-towed magnetic surv
Externí odkaz:
https://doaj.org/article/9b9f73f3b8c54291a632a2af11b11d8c
By checking the magnetic data measured from New Ocean Reacher 3 at 2020/9/21 to 29, we can easily find that there are two anomalies localized south-west of Penghu. In the west, it is located around 119.08°E, 23.46°N and with defect amount 620 nT. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::83375911f52ee6b6d25b3b280e4c4925
https://doi.org/10.5194/egusphere-egu23-4843
https://doi.org/10.5194/egusphere-egu23-4843
Autor:
Chung-Liang Lo, Shu-Kun Hsu, Shiao-Shan Lin, Ching-Hui Tsai, Wen-Bin Doo, Song-Chuen Chen, Pin-Ju Su
As an active mountain building, Taiwan Island is deduced from the oblique collision between the Eurasian and the Philippine Sea plate, and its northern part and offshore region are under post-collision collapse. The magmatism induced from the post-co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8eb5024b2be4103c04add66394a91321
https://doi.org/10.5194/egusphere-egu23-7718
https://doi.org/10.5194/egusphere-egu23-7718
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:
Yi Jung Lin, Shu Kun Hsu, Ching-Hui Tsai, Shiao Shan Lin, Hsueh Fen Wang, Chin Wei Liang, Wen Bin Doo, Chung Liang Lo, Yin Sheng Huang
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 30, Iss 5, Pp 675-683 (2019)
The Okinawa Trough (OT) is widely recognized as an area with extensive volcanism and hydrothermal activity. However, finding new hydrothermal vent sites in this region remains a technical challenge due to their small sizes. A deep-towed magnetic surv
Arc-continent collision and post-orogenic extension are both currently in progress in different parts of the Taiwan mountain belt. In particular, the junction of eastern Taiwan and the southernmost Ryukyu arc-trench system is a complex tectonic regio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b05da041212bd91c8f1c226120fe8b31
https://doi.org/10.5194/egusphere-egu2020-2249
https://doi.org/10.5194/egusphere-egu2020-2249
The subduction zone is a convergent plate boundary, and where most seismic activity is concentrated and megathrust may occur. To evaluate the potential hazard in subduction zones always relates to the plate coupling status. From previous studies, the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::db2a85499fb56f1187c85e58f03c38ae
https://doi.org/10.5194/egusphere-egu2020-18448
https://doi.org/10.5194/egusphere-egu2020-18448