Active Faults Of Central Taiwan

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Active Faults Of Central Taiwan

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Author : Chii-Wen Lin
language : zh-CN
Publisher:
Release Date : 2008

Active Faults Of Central Taiwan written by Chii-Wen Lin and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2008 with categories.

An Introduction To The Active Faults Of Taiwan

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Author : Hui-Cheng Chang
language : zh-CN
Publisher:
Release Date : 1998

An Introduction To The Active Faults Of Taiwan written by Hui-Cheng Chang and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 1998 with Faults (Geology) categories.

An Introduction To The Active Faults Of Taiwan

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Author :
language : en
Publisher:
Release Date : 2000

An Introduction To The Active Faults Of Taiwan written by and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2000 with categories.

A Review Of Recently Active Faults In Taiwan

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Author : Manuel G. Bonilla
language : en
Publisher:
Release Date : 1975

A Review Of Recently Active Faults In Taiwan written by Manuel G. Bonilla and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 1975 with Faults (Geology) categories.

Active Structural Growth In Central Taiwan In Relationship To Large Earthquakes And Pore Fluid Pressures

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Author : Li-Fan Yue
language : en
Publisher:
Release Date : 2007

Active Structural Growth In Central Taiwan In Relationship To Large Earthquakes And Pore Fluid Pressures written by Li-Fan Yue and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2007 with categories.

Central Taiwan is subject to a substantial long-term earthquake risk with a population of five million and two disastrous earthquakes in the last century, the 1935 ML=7.1 Tuntzuchiao and 1999 Mw=7.6 Chi-Chi earthquakes. Rich data from these earthquakes combined with substantial surface and subsurface data accumulated from petroleum exploration form the basis for these studies of the growth of structures in successive large earthquakes and their relationships to pore-fluid pressures.

A Geomorphological Study Of Active Faults In Taiwan

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Author : Tsai-Tien Shih
language : en
Publisher:
Release Date : 1977*

A Geomorphological Study Of Active Faults In Taiwan written by Tsai-Tien Shih and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 1977* with categories.

Acitve Faults Of Eastern And Southern Taiwan

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Author : Chii-Wen Lin
language : zh-CN
Publisher:
Release Date : 2009

Acitve Faults Of Eastern And Southern Taiwan written by Chii-Wen Lin and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2009 with categories.

Unveiling Active Faults Multiscale Perspectives And Alternative Approaches Addressing The Seismic Hazard Challenge

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Author : Federica Ferrarini
language : en
Publisher: Frontiers Media SA
Release Date : 2021-09-24

Unveiling Active Faults Multiscale Perspectives And Alternative Approaches Addressing The Seismic Hazard Challenge written by Federica Ferrarini and has been published by Frontiers Media SA this book supported file pdf, txt, epub, kindle and other format this book has been release on 2021-09-24 with Science categories.

Atlas Of Landsat Imagery Of Main Active Fault Zones In China

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Author :
language : en
Publisher:
Release Date : 1990

Atlas Of Landsat Imagery Of Main Active Fault Zones In China written by and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 1990 with Science categories.

Crustal Structure In Central And Northern Taiwan From Receiver Functions

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Author : Danielle Glasgow Wolf
language : en
Publisher:
Release Date : 2012

Crustal Structure In Central And Northern Taiwan From Receiver Functions written by Danielle Glasgow Wolf and has been published by this book supported file pdf, txt, epub, kindle and other format this book has been release on 2012 with categories.

Taiwan is the type-example of arc-continent collision, with the Luzon Arc on the oceanic Philippine Sea Plate (PSP) colliding with the continental margin of the Eurasian Plate (EUP). In this three-dimensionally complex convergence zone, the PSP subducts to the north beneath the EUP off of northeastern Taiwan, while the EUP subducts to the east beneath the PSP in central and southern Taiwan. The resulting accretion of the Philippine arc crust to the Eurasian continental margin exemplifies an important process in the growth of continents, yet the geometry and structure of the lithosphere at depth are poorly constrained. Some models of the Taiwan orogen propose that thin-skinned deformation above a basal décollement is the dominant deformational style, while other models suggest lithospheric-scale deformation and crustal thickening. This study, conducted as part of the TAiwan Integrated GEophysical Research (TAIGER) project, uses P and S wave receiver functions calculated from teleseismic earthquake data recorded at 30 broadband seismic stations deployed across northern and central Taiwan to detect lithospheric structure and further constrain the style of deformation at the Taiwan orogen. P wave receiver functions suggest the presence of a detachment fault in western central Taiwan continuing eastward from the Western foothills through the Hsueshan Range, and past the Lishan Fault into the Western Central Range. In central Taiwan, P and S wave receiver functions indicate that the crust thickens to the east, with estimated Moho depths increasing from approximately 29 km on the western coast to ~50 km beneath the Central Ranges. On the western coast of northern Taiwan, receiver functions yield an estimated Moho depth of approximately 23 km, with Moho depths increasing to ~40 - 45 km beneath north-central Taiwan. S wave receiver functions indicate that the depth to the base of the Eurasian slab beneath central Taiwan increases from ~100 km beneath the Coastal Plain in the west to ~165 km beneath central Taiwan. The base of the PSP lithosphere beneath eastern central Taiwan is estimated at ~120 km. These new estimates of crustal structure imply thinskinned deformation above a crustal-scale detachment in western Taiwan, with a transition to thicker crust and thick-skinned deformation in central and eastern Taiwan beneath the Hsueshan and Central Ranges.