Taiwan model: Combination of MT and seismicity

Chow Son Chen; Chein Chih Chen

Taiwan model: Combination of MT and seismicity

地球科學學系

研究成果: 會議貢獻類型 › 會議論文 › 同行評審

摘要

A strong correlation between the relevant seismic image and the geoelectric model of Taiwan, thus electrical conductivity image is interpreted with the constraints afforded by velocity information. The results show that both the velocity profile and the resistivity section indicate the slab of the subducting Philippine Sea plate. The conductive surface of the slab is thought to be related to fluids associated with the surface of the subducting plate. The slab northward deepens near latitude of 24°N to a depth of 50 km at the northern tip of Taiwan. The angle of subduction is interpreted to be 30º. At the depth of the Moho discontinuity, 40 km, a corresponding sharp boundary can be traced either from the conductivity profile or from the reflectivity section.

原文	???core.languages.en_GB???
出版狀態	已出版 - 1998
事件	1998 Society of Exploration Geophysicists Annual Meeting, SEG 1998 - New Orleans, United States 持續時間: 13 9月 1998 → 18 9月 1998

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???event.eventtypes.event.conference???	1998 Society of Exploration Geophysicists Annual Meeting, SEG 1998
國家/地區	United States
城市	New Orleans
期間	13/09/98 → 18/09/98

引用此

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abstract = "A strong correlation between the relevant seismic image and the geoelectric model of Taiwan, thus electrical conductivity image is interpreted with the constraints afforded by velocity information. The results show that both the velocity profile and the resistivity section indicate the slab of the subducting Philippine Sea plate. The conductive surface of the slab is thought to be related to fluids associated with the surface of the subducting plate. The slab northward deepens near latitude of 24°N to a depth of 50 km at the northern tip of Taiwan. The angle of subduction is interpreted to be 30º. At the depth of the Moho discontinuity, 40 km, a corresponding sharp boundary can be traced either from the conductivity profile or from the reflectivity section.",

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T2 - 1998 Society of Exploration Geophysicists Annual Meeting, SEG 1998

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AU - Chen, Chein Chih

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N2 - A strong correlation between the relevant seismic image and the geoelectric model of Taiwan, thus electrical conductivity image is interpreted with the constraints afforded by velocity information. The results show that both the velocity profile and the resistivity section indicate the slab of the subducting Philippine Sea plate. The conductive surface of the slab is thought to be related to fluids associated with the surface of the subducting plate. The slab northward deepens near latitude of 24°N to a depth of 50 km at the northern tip of Taiwan. The angle of subduction is interpreted to be 30º. At the depth of the Moho discontinuity, 40 km, a corresponding sharp boundary can be traced either from the conductivity profile or from the reflectivity section.

AB - A strong correlation between the relevant seismic image and the geoelectric model of Taiwan, thus electrical conductivity image is interpreted with the constraints afforded by velocity information. The results show that both the velocity profile and the resistivity section indicate the slab of the subducting Philippine Sea plate. The conductive surface of the slab is thought to be related to fluids associated with the surface of the subducting plate. The slab northward deepens near latitude of 24°N to a depth of 50 km at the northern tip of Taiwan. The angle of subduction is interpreted to be 30º. At the depth of the Moho discontinuity, 40 km, a corresponding sharp boundary can be traced either from the conductivity profile or from the reflectivity section.

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Y2 - 13 September 1998 through 18 September 1998

ER -

Taiwan model: Combination of MT and seismicity

摘要

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