Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Shiuh-Tsann Huang"'
Autor:
Maryline Le Béon, Mong-Han Huang, John Suppe, Shiuh-Tsann Huang, Erwan Pathier, Wen-Jeng Huang, Chien-Liang Chen, Bénédicte Fruneau, Stéphane Baize, Kuo-En Ching, Jyr-Ching Hu
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 28, Iss 5, Pp 663-681 (2017)
The Meinong earthquake generated up to ~10 cm surface displacement located 10 - 35 km west of the epicenter and monitored by InSAR and GPS. In addition to coseismic deformation related to the deep earthquake source, InSAR revealed three sharp surface
Externí odkaz:
https://doaj.org/article/4f7b89ec97204715980a4ce6b8a3929d
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 20, Iss 6, p 779 (2009)
The goal of this paper is to improve the capability of gravity inversion assessment of complex structures using a multiple-source model as indicated by a study of a foothill belt of north western Taiwan. In this study, a gravity inversion computer pr
Externí odkaz:
https://doaj.org/article/be51d010572940e388a643af160b0a9b
Autor:
Jong-Chang Wu, Shiuh-Tsann Huang, Ming-Huei Wang, Chin-Chun Tsai, Wen-Wei Mei, Jih-Hao Hung, Tung- Yi Lee, Kenn-Ming Yang, Kun-Fa Lee
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 18, Iss 2, p 295 (2007)
The results of this nannofossil analysis supply essential information for determining the formation boundaries in the upper Pliocene to Pleistocene. These results also verify the existence of a repetition fossil zone.
Externí odkaz:
https://doaj.org/article/60f0b9fe13ad4796897dcaa757a2e3af
Autor:
Kenn-Ming Yang, Shiuh-Tsann Huang, Jong-Chang Wu, Hsin-Hsiu Ting, Wen-Wei Mei, Min Lee, Hsiang-Horng Hsu, Chang-Jie Lee
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences, Vol 18, Iss 2, p 143 (2007)
This study is aimed at constructing a 3D subsurface geometry of the Chelungpu thrust and its associated structures, as well as examining the implications of the studies results for active tectonics in the area. Nine balanced cross-sections were const
Externí odkaz:
https://doaj.org/article/2fb15395734645ba909bce1a2624861a
Autor:
Shiuh-Tsann Huang, 黃旭燦
92
This study will be focused on the analysis of regional mesoscopic structural framework as well as the analysis of active faults in central and southern Taiwan. Three areas were chosen for structure analysis in order to decipher their geometri
This study will be focused on the analysis of regional mesoscopic structural framework as well as the analysis of active faults in central and southern Taiwan. Three areas were chosen for structure analysis in order to decipher their geometri
Externí odkaz:
http://ndltd.ncl.edu.tw/handle/05334447219243696059
Autor:
Ruey Juin Rau, Kenn Ming Yang, Shiuh Tsann Huang, Yi Jin Tang, Ching Yun Hsieh, Hsin Hsiu Ting, Hao Yun Chang, Jong Chang Wu
Publikováno v:
Geological Magazine. 153:1166-1191
In the foreland area of western Taiwan, some of the pre-orogenic basement-involved normal faults were reactivated during the subsequent compressional tectonics. The main purpose of this paper is to investigate the role played by the pre-existing norm
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::54e7a3fc95a8844fdd9bea0b28cdb5df
https://doi.org/10.1017/s0016756816000637
https://doi.org/10.1017/s0016756816000637
Autor:
Jyr-Ching Hu, Chien Liang Chen, John Suppe, Shiuh Tsann Huang, Wen Jeng Huang, Kuo En Ching, Maryline Le Béon, Stéphane Baize, Erwan Pathier, Mong-Han Huang, Bénédicte Fruneau
Publikováno v:
Terrestrial, Atmospheric and Oceanic Sciences
Terrestrial, Atmospheric and Oceanic Sciences, 2017, 28 (5), ⟨10.3319/TAO.2017.03.20.02⟩
Terrestrial, Atmospheric and Oceanic Sciences, Vol 28, Iss 5, Pp 663-681 (2017)
Terrestrial, Atmospheric and Oceanic Sciences, 2017, 28 (5), ⟨10.3319/TAO.2017.03.20.02⟩
Terrestrial, Atmospheric and Oceanic Sciences, Vol 28, Iss 5, Pp 663-681 (2017)
International audience; The Meinong earthquake generated up to ∼10 cm surface displacement located 10-35 km W of the epicenter and monitored by InSAR and GPS. In addition to coseismic deformation related to the deep earthquake source, InSAR reveale
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a1ef8c4236f768798d69779b75928a75
https://hal.archives-ouvertes.fr/hal-02555519
https://hal.archives-ouvertes.fr/hal-02555519
Autor:
Brian J. Yanites, Shiuh Tsann Huang, Karl Mueller, L.K. Powell, Yue-Gau Chen, Phaedra Upton, T. Wilcox, Gregory E. Tucker
Publikováno v:
Geosphere. 9:1091-1101
Late Quaternary shortening along the length of the Western Foothills of Taiwan highlights the tectonic segmentation of the foreland and raises questions about the relationship between erosion and the thickness of synorogenic foreland basin fill, and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37c3d05b90f43376c440fc42ef8d6b1d
https://doi.org/10.1130/ges00819.1
https://doi.org/10.1130/ges00819.1
Autor:
Ching-Hua Lo, Kuo-Lung Wang, Yi Ming Lo, Shiuh Tsann Huang, Sun-Lin Chung, Ryuichi Shinjo, Tung Yi Lee, Huai Jen Yang, Jong Chang Wu
Publikováno v:
Lithos. 155:426-441
The southeastern Eurasian continental margin has been characterized by formation of rift basins associated with intraplate basaltic volcanism since early Cenozoic time. In contrast to Paleogene volcanic rocks that occur sporadically in the basins, Ne
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::48cc03037bf35fe7740dec600e657fc6
https://doi.org/10.1016/j.lithos.2012.10.002
https://doi.org/10.1016/j.lithos.2012.10.002
Publikováno v:
International Geology Review. 48:910-941
Taiwan is located on the boundary between the Eurasian and Philippine Sea plates. As a result, foreland tectonics in western Taiwan can be divided into two domains: pre-orogenic extensional structures and those of the outer part of the fold-and-thrus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::59c9045e5d5d13f3293f65101b64d10f
https://doi.org/10.2747/0020-6814.48.10.910
https://doi.org/10.2747/0020-6814.48.10.910