Zobrazeno 1 - 10
of 234
pro vyhledávání: '"Cheng-Horng Lin"'
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 34, Iss 1, Pp 1-15 (2023)
Abstract The Taiwan orogenic belt is formed by the strong convergence between the Philippine Sea Plate and the Eurasian Plate. The detailed mountain building process is still under debated largely due to the poor constraint of deep crustal structures
Externí odkaz:
https://doaj.org/article/08b583dec6214def96106cac3b2509a5
Autor:
Kate Huihsuan Chen, Ting-Chen Yeh, Yaochieh Chen, Christopher W. Johnson, Cheng-Horng Lin, Ya-Chuan Lai, Min-Hung Shih, Philippe Guéguen, Win-Gee Huang, Bor-Shouh Huang, Kou-Cheng Chen, Chin-Jen Lin, Chin-Shang Ku
Publikováno v:
Scientific Reports, Vol 12, Iss 1, Pp 1-12 (2022)
Abstract Examining continuous seismic data recorded by a dense broadband seismic network throughout Taipei shows for the first time, the nature of seismic noise in this highly populated metropolitan area. Using 140 broadband stations in a 50 km × 69
Externí odkaz:
https://doaj.org/article/915ae30642024bd2a81c79e07e442398
Autor:
Chieh-Hung Chen, Yang-Yi Sun, Li-Ching Lin, Peng Han, Huai-Zhong Yu, XueMin Zhang, Chi-Chia Tang, Chun-Rong Chen, Horng-Yuan Yen, Cheng-Horng Lin, Jann-Yenq Liu, Ching-Ren Lin
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-8 (2021)
Abstract Acoustic-gravity waves are generally considered to be one of the major factors that drive changes of the total electron content in the ionosphere. However, causal mechanisms of couplings between sources in the lithosphere and responses in th
Externí odkaz:
https://doaj.org/article/099e4647bfbc414697137a49ca748a58
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-12 (2021)
Abstract It is conventionally believed that magma generation beneath the volcanic arc is triggered by the infiltration of fluids or melts derived from the subducted slab. However, recently geochemical analyses argue the arc magma may be formed by mé
Externí odkaz:
https://doaj.org/article/e431e17415d84967a86915e01369968e
Autor:
Chun-Rong Chen, Jann-Yenq Liu, Chieh-Hung Chen, Tsung-Yu Wu, Horng-Yuan Yen, Strong Wen, Bor-Shouh Huang, Cheng-Horng Lin, Che-Min Lin, Hung-Hao Hsieh
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 30, Iss 3, Pp 449-465 (2019)
The strong ground motion of 6 February 2018 M 6.2 Hualien Earthquake triggered a series of co-seismic geomagnetic fluctuations and seismo-traveling atmospheric disturbances (STADs) signatures in infrasonic waves and micro-pressures upon the seismic w
Externí odkaz:
https://doaj.org/article/5c5425dc90af49a5aae2f915b1b8176c
Autor:
Horng-Yue Chen, Ryoya Ikuta, Ya-Ju Hsu, Toshiaki Tsujii, Masataka Ando, Yoko Tu, Takeru Kohmi, Kiyomichi Takemoto, Koto Mizuno, Hsin Tung, Chin-Shang Ku, Cheng-Horng Lin
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Long-term seafloor geodetic measurements are important for constraining submarine crustal deformation near plate boundaries. Here we present an integrated analysis of a decade of GNSS/acoustic data collected at a site 60 km to the east of northeast T
Externí odkaz:
https://doaj.org/article/32f511bcb6764eb7a084091e6cbb1065
Publikováno v:
Seismological Research Letters. 94:617-625
The major eruption that occurred on 15 January 2022 on Hunga Tonga Hunga Ha’apai (HTHH) in Tonga generated powerful acoustic waves that propagated through the atmosphere all over the world. Although the eruption energy was soon estimated from the a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6b010cad3842a1c9bc7cbe2ac7771104
https://doi.org/10.1785/0220220233
https://doi.org/10.1785/0220220233
Publikováno v:
Scientific Reports, Vol 8, Iss 1, Pp 1-12 (2018)
Abstract Although surface geology, eruption information and clustering seismicity all suggest Turtle Island (Kueishantao) of northern Taiwan is an active volcano, there was no direct evidence to conclude that magma reservoirs exist beneath it. Even l
Externí odkaz:
https://doaj.org/article/7f914e4377b747f4844cd233172b0f21
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 29, Iss 5, Pp 499-508 (2018)
Taiwan is one of the most typical arc-continental collision systems in the world. The Taiwan orogeny is often explained by the thin-skin model, where a shallow decollement, with depths of less than 10 km, is considered as the crustal deformation boun
Externí odkaz:
https://doaj.org/article/960ba44af0944af7b5266b0e268d1414
Autor:
Arvind Kumar, Vivek Walia, Yi-Chun Sung, Shih-Jung Lin, Hasio-Fen Lee, Cheng-Horng Lin, Ching-Chou Fu, Cheng-Hong Chen
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 29, Iss 3, Pp 261-273 (2018)
Taiwan is highly active tectonically and intensively faulted resulting in occurrence of number of big earthquakes in the region. In the northern part of Taiwan Island, a group of volcanoes are distributed. These volcanoes are known as the Tatun volca
Externí odkaz:
https://doaj.org/article/b9d593352fe1428faeeaafadc8ef2eb0