M
Meng-Long Hsieh
Researcher at National Chung Cheng University
Publications - 24
Citations - 635
Meng-Long Hsieh is an academic researcher from National Chung Cheng University. The author has contributed to research in topics: Fluvial & River terraces. The author has an hindex of 13, co-authored 24 publications receiving 578 citations. Previous affiliations of Meng-Long Hsieh include Binghamton University & National Taiwan University.
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Modern vertical deformation rates and mountain building in Taiwan from precise leveling and continuous GPS observations, 2000–2008
TL;DR: In this article, the present-day and geologic vertical displacement field in the active Taiwan orogenic belt was characterized using GPS vertical velocities and precise leveling and 199 continuous GPS measurements from 2000 to 2008.
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Middle–late Holocene river terraces in the Erhjen River Basin, southwestern Taiwan—implications of river response to climate change and active tectonic uplift
TL;DR: In this paper, the authors reconstruct the Holocene river history of the Erhjen River (area: 140 km 2 ) by correlating river terraces aided by 28 radiocarbon dates.
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Slip vectors of the surface rupture of the 1999 Chi-Chi earthquake, western Taiwan
Yuan-Hsi Lee,Meng-Long Hsieh,Shih-Ding Lu,Tung-Sheng Shih,Wei-Yu Wu,Yuichi Sugiyama,Takashi Azuma,Yoshihiko Kariya +7 more
TL;DR: In this paper, 100 slip vectors were surveyed along the 1999 Chi-Chi earthquake rupture (100 km long), western Taiwan, to understand the coseismic reverse-faulting processes The surveyed slip azimuths vary locally (over 80°) where the rupture is irregular or associated with flexure.
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Holocene tectonic uplift deduced from elevated shorelines, eastern Coastal Range of Taiwan
P.M. Liew,Paolo Antonio Pirazzoli,Meng-Long Hsieh,Maurice Arnold,J.P. Barusseau,Michel Fontugne,P. Giresse +6 more
TL;DR: In this article, the tectonic trends that can be deduced from the Holocene raised shorelines between Ch'eng-kung and Hsin-she, along a 65-km long coastal sector in the eastern Coastal Range of Taiwan are investigated.
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Late Holocene (2 ka) sea level, river discharge and climate interrelationship in the Taiwan region
Ping.-Mei Liew,Meng-Long Hsieh +1 more
TL;DR: Based on the palynological study of two alpine lakes of the central mountains and a lake at 460m elevation in northeastern Taiwan, a warm event which lasted several hundred years from about cal 2 ka, followed a cool-dry interval from about Cal 3.7-2.0 ka as discussed by the authors.