Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan

Based on seismic reflection profiles and multi-beam bathymetric data, a large submarine landslide named Fangliao Slide is mapped for the first time off SW Taiwan. The Fangliao Slide occurred on the continental slope to the west of the Fangliao Canyon at water depths between 420 and 900 m. The seaflo...
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Autor*in:	Song-Chuen Chen [verfasserIn] Ching-Hui Tsai [verfasserIn] Shu-Kun Hsu [verfasserIn] Yi-Ching Yeh [verfasserIn] Char-Shine Liu [verfasserIn] San-Hsiung Chung [verfasserIn] Cheng-Yueh Wei [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2018

Übergeordnetes Werk:	In: Terrestrial, Atmospheric and Oceanic Sciences - Springer, 2016, 29(2018), 1, Seite 17-30
Übergeordnetes Werk:	volume:29 ; year:2018 ; number:1 ; pages:17-30

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.3319/TAO.2017.06.14.01

Katalog-ID:	DOAJ040763757

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520			\|a Based on seismic reflection profiles and multi-beam bathymetric data, a large submarine landslide named Fangliao Slide is mapped for the first time off SW Taiwan. The Fangliao Slide occurred on the continental slope to the west of the Fangliao Canyon at water depths between 420 and 900 m. The seafloor of the Fangliao Slide has a gentle slope angle (~1 - 2°). The landslide covers an area of ~15 km length and ~10 km width and a volume of ~26 km3. The headwall of the landslide has ~30 m vertical offset at the southern flank of mud diapir MD7-1, and the sidewalls are bounded by fault A in the west and faults C and D in the east. The sliding area is composed of five bathymetric terraces, indicating that the slope failures have occurred several times. The Fangliao Slide can be divided into an upper domain and a lower domain, separated at the water depth of ~600 m where the gas hydrate off SW Taiwan becomes dissociate. The initial slope failure of the Fangliao Slide was probably linked to mud diapirism of MD7-1 and the slope failure in the lower domain was probably augmented by the gas hydrate dissociation. The seafloor morphology in the lower domain is therefore more corrugated than in the upper domain.
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spelling	10.3319/TAO.2017.06.14.01 doi (DE-627)DOAJ040763757 (DE-599)DOAJa0217117aa174469bfa12919094d1b5d DE-627 ger DE-627 rakwb eng QE1-996.5 QC801-809 Song-Chuen Chen verfasserin aut Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Based on seismic reflection profiles and multi-beam bathymetric data, a large submarine landslide named Fangliao Slide is mapped for the first time off SW Taiwan. The Fangliao Slide occurred on the continental slope to the west of the Fangliao Canyon at water depths between 420 and 900 m. The seafloor of the Fangliao Slide has a gentle slope angle (~1 - 2°). The landslide covers an area of ~15 km length and ~10 km width and a volume of ~26 km3. The headwall of the landslide has ~30 m vertical offset at the southern flank of mud diapir MD7-1, and the sidewalls are bounded by fault A in the west and faults C and D in the east. The sliding area is composed of five bathymetric terraces, indicating that the slope failures have occurred several times. The Fangliao Slide can be divided into an upper domain and a lower domain, separated at the water depth of ~600 m where the gas hydrate off SW Taiwan becomes dissociate. The initial slope failure of the Fangliao Slide was probably linked to mud diapirism of MD7-1 and the slope failure in the lower domain was probably augmented by the gas hydrate dissociation. The seafloor morphology in the lower domain is therefore more corrugated than in the upper domain. Geology Geophysics. Cosmic physics Ching-Hui Tsai verfasserin aut Shu-Kun Hsu verfasserin aut Yi-Ching Yeh verfasserin aut Char-Shine Liu verfasserin aut San-Hsiung Chung verfasserin aut Cheng-Yueh Wei verfasserin aut In Terrestrial, Atmospheric and Oceanic Sciences Springer, 2016 29(2018), 1, Seite 17-30 (DE-627)527829951 (DE-600)2278841-4 23117680 nnns volume:29 year:2018 number:1 pages:17-30 https://doi.org/10.3319/TAO.2017.06.14.01 kostenfrei https://doaj.org/article/a0217117aa174469bfa12919094d1b5d kostenfrei http://tao.cgu.org.tw/media/k2/attachments/v291p017.pdf kostenfrei https://doaj.org/toc/1017-0839 Journal toc kostenfrei https://doaj.org/toc/2311-7680 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 29 2018 1 17-30
allfields_unstemmed	10.3319/TAO.2017.06.14.01 doi (DE-627)DOAJ040763757 (DE-599)DOAJa0217117aa174469bfa12919094d1b5d DE-627 ger DE-627 rakwb eng QE1-996.5 QC801-809 Song-Chuen Chen verfasserin aut Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Based on seismic reflection profiles and multi-beam bathymetric data, a large submarine landslide named Fangliao Slide is mapped for the first time off SW Taiwan. The Fangliao Slide occurred on the continental slope to the west of the Fangliao Canyon at water depths between 420 and 900 m. The seafloor of the Fangliao Slide has a gentle slope angle (~1 - 2°). The landslide covers an area of ~15 km length and ~10 km width and a volume of ~26 km3. The headwall of the landslide has ~30 m vertical offset at the southern flank of mud diapir MD7-1, and the sidewalls are bounded by fault A in the west and faults C and D in the east. The sliding area is composed of five bathymetric terraces, indicating that the slope failures have occurred several times. The Fangliao Slide can be divided into an upper domain and a lower domain, separated at the water depth of ~600 m where the gas hydrate off SW Taiwan becomes dissociate. The initial slope failure of the Fangliao Slide was probably linked to mud diapirism of MD7-1 and the slope failure in the lower domain was probably augmented by the gas hydrate dissociation. The seafloor morphology in the lower domain is therefore more corrugated than in the upper domain. Geology Geophysics. Cosmic physics Ching-Hui Tsai verfasserin aut Shu-Kun Hsu verfasserin aut Yi-Ching Yeh verfasserin aut Char-Shine Liu verfasserin aut San-Hsiung Chung verfasserin aut Cheng-Yueh Wei verfasserin aut In Terrestrial, Atmospheric and Oceanic Sciences Springer, 2016 29(2018), 1, Seite 17-30 (DE-627)527829951 (DE-600)2278841-4 23117680 nnns volume:29 year:2018 number:1 pages:17-30 https://doi.org/10.3319/TAO.2017.06.14.01 kostenfrei https://doaj.org/article/a0217117aa174469bfa12919094d1b5d kostenfrei http://tao.cgu.org.tw/media/k2/attachments/v291p017.pdf kostenfrei https://doaj.org/toc/1017-0839 Journal toc kostenfrei https://doaj.org/toc/2311-7680 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 29 2018 1 17-30
allfieldsGer	10.3319/TAO.2017.06.14.01 doi (DE-627)DOAJ040763757 (DE-599)DOAJa0217117aa174469bfa12919094d1b5d DE-627 ger DE-627 rakwb eng QE1-996.5 QC801-809 Song-Chuen Chen verfasserin aut Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Based on seismic reflection profiles and multi-beam bathymetric data, a large submarine landslide named Fangliao Slide is mapped for the first time off SW Taiwan. The Fangliao Slide occurred on the continental slope to the west of the Fangliao Canyon at water depths between 420 and 900 m. The seafloor of the Fangliao Slide has a gentle slope angle (~1 - 2°). The landslide covers an area of ~15 km length and ~10 km width and a volume of ~26 km3. The headwall of the landslide has ~30 m vertical offset at the southern flank of mud diapir MD7-1, and the sidewalls are bounded by fault A in the west and faults C and D in the east. The sliding area is composed of five bathymetric terraces, indicating that the slope failures have occurred several times. The Fangliao Slide can be divided into an upper domain and a lower domain, separated at the water depth of ~600 m where the gas hydrate off SW Taiwan becomes dissociate. The initial slope failure of the Fangliao Slide was probably linked to mud diapirism of MD7-1 and the slope failure in the lower domain was probably augmented by the gas hydrate dissociation. The seafloor morphology in the lower domain is therefore more corrugated than in the upper domain. Geology Geophysics. Cosmic physics Ching-Hui Tsai verfasserin aut Shu-Kun Hsu verfasserin aut Yi-Ching Yeh verfasserin aut Char-Shine Liu verfasserin aut San-Hsiung Chung verfasserin aut Cheng-Yueh Wei verfasserin aut In Terrestrial, Atmospheric and Oceanic Sciences Springer, 2016 29(2018), 1, Seite 17-30 (DE-627)527829951 (DE-600)2278841-4 23117680 nnns volume:29 year:2018 number:1 pages:17-30 https://doi.org/10.3319/TAO.2017.06.14.01 kostenfrei https://doaj.org/article/a0217117aa174469bfa12919094d1b5d kostenfrei http://tao.cgu.org.tw/media/k2/attachments/v291p017.pdf kostenfrei https://doaj.org/toc/1017-0839 Journal toc kostenfrei https://doaj.org/toc/2311-7680 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 29 2018 1 17-30
allfieldsSound	10.3319/TAO.2017.06.14.01 doi (DE-627)DOAJ040763757 (DE-599)DOAJa0217117aa174469bfa12919094d1b5d DE-627 ger DE-627 rakwb eng QE1-996.5 QC801-809 Song-Chuen Chen verfasserin aut Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Based on seismic reflection profiles and multi-beam bathymetric data, a large submarine landslide named Fangliao Slide is mapped for the first time off SW Taiwan. The Fangliao Slide occurred on the continental slope to the west of the Fangliao Canyon at water depths between 420 and 900 m. The seafloor of the Fangliao Slide has a gentle slope angle (~1 - 2°). The landslide covers an area of ~15 km length and ~10 km width and a volume of ~26 km3. The headwall of the landslide has ~30 m vertical offset at the southern flank of mud diapir MD7-1, and the sidewalls are bounded by fault A in the west and faults C and D in the east. The sliding area is composed of five bathymetric terraces, indicating that the slope failures have occurred several times. The Fangliao Slide can be divided into an upper domain and a lower domain, separated at the water depth of ~600 m where the gas hydrate off SW Taiwan becomes dissociate. The initial slope failure of the Fangliao Slide was probably linked to mud diapirism of MD7-1 and the slope failure in the lower domain was probably augmented by the gas hydrate dissociation. The seafloor morphology in the lower domain is therefore more corrugated than in the upper domain. Geology Geophysics. Cosmic physics Ching-Hui Tsai verfasserin aut Shu-Kun Hsu verfasserin aut Yi-Ching Yeh verfasserin aut Char-Shine Liu verfasserin aut San-Hsiung Chung verfasserin aut Cheng-Yueh Wei verfasserin aut In Terrestrial, Atmospheric and Oceanic Sciences Springer, 2016 29(2018), 1, Seite 17-30 (DE-627)527829951 (DE-600)2278841-4 23117680 nnns volume:29 year:2018 number:1 pages:17-30 https://doi.org/10.3319/TAO.2017.06.14.01 kostenfrei https://doaj.org/article/a0217117aa174469bfa12919094d1b5d kostenfrei http://tao.cgu.org.tw/media/k2/attachments/v291p017.pdf kostenfrei https://doaj.org/toc/1017-0839 Journal toc kostenfrei https://doaj.org/toc/2311-7680 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 29 2018 1 17-30
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authorswithroles_txt_mv	Song-Chuen Chen @@aut@@ Ching-Hui Tsai @@aut@@ Shu-Kun Hsu @@aut@@ Yi-Ching Yeh @@aut@@ Char-Shine Liu @@aut@@ San-Hsiung Chung @@aut@@ Cheng-Yueh Wei @@aut@@
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callnumber-first	Q - Science
author	Song-Chuen Chen
spellingShingle	Song-Chuen Chen misc QE1-996.5 misc QC801-809 misc Geology misc Geophysics. Cosmic physics Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan
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topic_title	QE1-996.5 QC801-809 Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan
topic	misc QE1-996.5 misc QC801-809 misc Geology misc Geophysics. Cosmic physics
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title	Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan
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title_full	Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan
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title_sort	fangliao slide — a large slope failure in the upper kaoping slope off southwest taiwan
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title_auth	Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan
abstract	Based on seismic reflection profiles and multi-beam bathymetric data, a large submarine landslide named Fangliao Slide is mapped for the first time off SW Taiwan. The Fangliao Slide occurred on the continental slope to the west of the Fangliao Canyon at water depths between 420 and 900 m. The seafloor of the Fangliao Slide has a gentle slope angle (~1 - 2°). The landslide covers an area of ~15 km length and ~10 km width and a volume of ~26 km3. The headwall of the landslide has ~30 m vertical offset at the southern flank of mud diapir MD7-1, and the sidewalls are bounded by fault A in the west and faults C and D in the east. The sliding area is composed of five bathymetric terraces, indicating that the slope failures have occurred several times. The Fangliao Slide can be divided into an upper domain and a lower domain, separated at the water depth of ~600 m where the gas hydrate off SW Taiwan becomes dissociate. The initial slope failure of the Fangliao Slide was probably linked to mud diapirism of MD7-1 and the slope failure in the lower domain was probably augmented by the gas hydrate dissociation. The seafloor morphology in the lower domain is therefore more corrugated than in the upper domain.
abstractGer	Based on seismic reflection profiles and multi-beam bathymetric data, a large submarine landslide named Fangliao Slide is mapped for the first time off SW Taiwan. The Fangliao Slide occurred on the continental slope to the west of the Fangliao Canyon at water depths between 420 and 900 m. The seafloor of the Fangliao Slide has a gentle slope angle (~1 - 2°). The landslide covers an area of ~15 km length and ~10 km width and a volume of ~26 km3. The headwall of the landslide has ~30 m vertical offset at the southern flank of mud diapir MD7-1, and the sidewalls are bounded by fault A in the west and faults C and D in the east. The sliding area is composed of five bathymetric terraces, indicating that the slope failures have occurred several times. The Fangliao Slide can be divided into an upper domain and a lower domain, separated at the water depth of ~600 m where the gas hydrate off SW Taiwan becomes dissociate. The initial slope failure of the Fangliao Slide was probably linked to mud diapirism of MD7-1 and the slope failure in the lower domain was probably augmented by the gas hydrate dissociation. The seafloor morphology in the lower domain is therefore more corrugated than in the upper domain.
abstract_unstemmed	Based on seismic reflection profiles and multi-beam bathymetric data, a large submarine landslide named Fangliao Slide is mapped for the first time off SW Taiwan. The Fangliao Slide occurred on the continental slope to the west of the Fangliao Canyon at water depths between 420 and 900 m. The seafloor of the Fangliao Slide has a gentle slope angle (~1 - 2°). The landslide covers an area of ~15 km length and ~10 km width and a volume of ~26 km3. The headwall of the landslide has ~30 m vertical offset at the southern flank of mud diapir MD7-1, and the sidewalls are bounded by fault A in the west and faults C and D in the east. The sliding area is composed of five bathymetric terraces, indicating that the slope failures have occurred several times. The Fangliao Slide can be divided into an upper domain and a lower domain, separated at the water depth of ~600 m where the gas hydrate off SW Taiwan becomes dissociate. The initial slope failure of the Fangliao Slide was probably linked to mud diapirism of MD7-1 and the slope failure in the lower domain was probably augmented by the gas hydrate dissociation. The seafloor morphology in the lower domain is therefore more corrugated than in the upper domain.
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title_short	Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan
url	https://doi.org/10.3319/TAO.2017.06.14.01 https://doaj.org/article/a0217117aa174469bfa12919094d1b5d http://tao.cgu.org.tw/media/k2/attachments/v291p017.pdf https://doaj.org/toc/1017-0839 https://doaj.org/toc/2311-7680
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up_date	2024-07-03T16:37:53.127Z
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The Fangliao Slide occurred on the continental slope to the west of the Fangliao Canyon at water depths between 420 and 900 m. The seafloor of the Fangliao Slide has a gentle slope angle (~1 - 2°). The landslide covers an area of ~15 km length and ~10 km width and a volume of ~26 km3. The headwall of the landslide has ~30 m vertical offset at the southern flank of mud diapir MD7-1, and the sidewalls are bounded by fault A in the west and faults C and D in the east. The sliding area is composed of five bathymetric terraces, indicating that the slope failures have occurred several times. The Fangliao Slide can be divided into an upper domain and a lower domain, separated at the water depth of ~600 m where the gas hydrate off SW Taiwan becomes dissociate. The initial slope failure of the Fangliao Slide was probably linked to mud diapirism of MD7-1 and the slope failure in the lower domain was probably augmented by the gas hydrate dissociation. 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Fangliao Slide — a large slope failure in the upper Kaoping Slope off southwest Taiwan

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