Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Wen-Rong Chi"'
Autor:
Romain Vaucher, Antoine Dillinger, Amy I. Hsieh, Wen‐Rong Chi, Ludvig Löwemark, Shahin E. Dashtgard
Publikováno v:
The Depositional Record, Vol 9, Iss 4, Pp 820-843 (2023)
Abstract Storm‐flood‐dominated deltas are sedimentary systems in which a complex interplay of hydrodynamic processes occurs during storms (e.g. tropical cyclones) due to the coeval action of continental and oceanic processes. This paper reports o
Externí odkaz:
https://doaj.org/article/c8c8cef170654004864d97a5cda95d6d
Autor:
Larry Syu-Heng Lai, Rebecca J. Dorsey, Chorng-Shern Horng, Wen-Rong Chi, Kai-Shuan Shea, Jiun-Yee Yen
Publikováno v:
Communications Earth & Environment, Vol 3, Iss 1, Pp 1-10 (2022)
Uplift and subsidence in island arcs during arc-continent collision may reach rates of over 14 mm per year, substantially faster than previously thought, according to stratigraphic analyses and sediment backstripping in Taiwan’s Coastal Range
Externí odkaz:
https://doaj.org/article/9284ee9d24c74bdba996415f1294fe6a
Autor:
Romain Vaucher, Shahin E. Dashtgard, Chorng-Shern Horng, Christian Zeeden, Antoine Dillinger, Yu-Yen Pan, Romy A. Setiaji, Wen-Rong Chi, Ludvig Löwemark
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-11 (2021)
Abstract Global marine archives from the early Pleistocene indicate that glacial-interglacial cycles, and their corresponding sea-level cycles, have predominantly a periodicity of ~ 41 kyrs driven by Earth’s obliquity. Here, we present a clastic sh
Externí odkaz:
https://doaj.org/article/732f1782b7254c5494ded9ef472aff35
Autor:
Larry Syu-Heng Lai, Rebecca Dorsey, Chorng-Shern Horng, Wen-Rong Chi, Kai-Shuan Shea, Jiun-Yee Yen
The Plio-Pleistocene Lichi Mélange in the Coastal Range of eastern Taiwan offers an excellent opportunity to study processes of mélange development at the continent-ocean interface of an active arc-continent collision. This paper presents new resul
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0876e76eb3e87e4c3ea791a995964896
https://doi.org/10.31223/x5hp5v
https://doi.org/10.31223/x5hp5v
Autor:
Shahin E. Dashtgard, Romain Vaucher, Wen-Rong Chi, Yu-Yen Pan, Antoine Dillinger, Ludvig Löwemark, Chorng-Shern Horng, Romy A. Setiaji, Christian Zeeden
The Pleistocene was a phase of global cooling of the Earth through which glacial-interglacial cycles occurred, and the growth and decay of the ice-sheets resulted in quasi-cyclic sea-level fluctuations driven by orbital forcing. Despite that summer i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b6d1effe44c681d10eaafe4ab5415b7
https://doi.org/10.5194/egusphere-egu21-1433
https://doi.org/10.5194/egusphere-egu21-1433
Autor:
Wen-Rong Chi, Rebecca J. Dorsey, Kai-Shuan Shea, Larry Syu-Heng Lai, Chorng-Shern Horng, Jiun-Yee Yen
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2e32c81b4d91ab63d72039a7f8cf5241
https://doi.org/10.1130/abs/2021am-365341
https://doi.org/10.1130/abs/2021am-365341
Autor:
Larry Syu-Heng Lai, Rebecca J. Dorsey, Kai-Shuan Shea, Wen-Rong Chi, Chorng-Shern Horng, Jiun-Yee Yen
Publikováno v:
Sedimentary Geology. 418:105901
The Plio-Pleistocene Lichi Melange in the Coastal Range of eastern Taiwan offers an excellent opportunity to study processes of melange development at the continent-ocean interface of an active arc-continent collision. This paper presents new results
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c25cb2b9a869027e580fe583941af8d1
https://doi.org/10.1016/j.sedgeo.2021.105901
https://doi.org/10.1016/j.sedgeo.2021.105901
Publikováno v:
Island Arc. 24:317-341
The overriding of the Luzon volcanic arc atop the underlying Chinese rifted-continental margin has caused the formation of the Taiwan mountain belts and a peripheral foreland basin west of the orogen since the late Miocene. In this study, lithofacies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd81a8ef97fb9850d78cc4b6058c379b
https://doi.org/10.1111/iar.12113
https://doi.org/10.1111/iar.12113
Autor:
Shou Yeh Gong, Jong Chang Wu, Tzen-Fu Yui, Chorng Sherng Horng, Wen Rong Chi, Shieu Tsann Huang, Kuo-Yen Wei, Horng Sheng Mii, Kenn Ming Yang, Fu Wen Huang, Shih-Wei Wang, Pei Keng Torng, Chen-Feng You
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 226:205-213
The Nansha (Spratly) Islands are located in the middle of the South China Sea (at about 10°N) near the northwestern margin of the Western Pacific Warm Pool (WPWP). A borehole was drilled at an atoll at Nansha, and cores were taken. The upper 165.4 m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e57b3dc1a507025cccd170c9d768118
https://doi.org/10.1016/j.palaeo.2005.05.012
https://doi.org/10.1016/j.palaeo.2005.05.012
Publikováno v:
Tectonics
A foreland basin system with its asymmetric basin geometry extends from the frontal areas of a mountain-building belt to the margin of craton and includes, as defined by DeCelles and Giles [1], wedge-top, foreland basin, forebulge and backbulge. Fore
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7f4aac519d7eae6b7bbeb796940f119a
http://www.intechopen.com/articles/show/title/tectonic-implications-of-stratigraphy-architecture-in-distal-part-of-foreland-basin-southwestern-tai
http://www.intechopen.com/articles/show/title/tectonic-implications-of-stratigraphy-architecture-in-distal-part-of-foreland-basin-southwestern-tai