review the 1906 meishan eart hquake and chiayi …review the 1906 meishan eart hquake and chiayi...

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Review the 1906 Meishan earthquake and Chiayi Transfer Zone in Central Taiwan Yuan-Hsi Lee National Chung-Cheng University Taiwan earthquake model 1906 Meishan earthquake ML:7.1 Chiayi area -Characteristics of the active faults fault length; dip angle; slip rate…. -Chiayi transfer structure

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  • Review the 1906 Meishan earthquake and Chiayi Transfer Zone in Central Taiwan

    Yuan-Hsi LeeNational Chung-Cheng University

    Taiwan earthquake model1906 Meishan earthquake ML:7.1Chiayi area

    -Characteristics of the active faultsfault length; dip angle; slip rate….

    -Chiayi transfer structure

  • 2001-2012

    2

  • Tectonics and Seismicity of Taiwan

    3

    1946

    1906

    1935

  • 1935

    1946

    1951

    1999

    1906

    Active transverse structure in fold and thrust belt of Taiwan

  • 1935:TuntzuchiaofaultShihtan faultShenchoshan faultML:7.1Death: 3279Injury:12119Totally destroyed

    houses:19729

  • 1935:Tuntzchiao fault

  • 1946:Hsinhwa fault

  • Date March 17, 1906 Meishan earthquakeMagnitude 7.1 MLcasualties 1,258 dead

    2,385 injured

  • At 5:12 a.m. on April 18, 1906Francisco earthquake

  • 1906 Meishan earthquake(Omori, 1907)

    Prof. Cheng

  • Coseismic displacement of the 1906 Meishan earthquake (Omori, 1907)

    uplift

    uplift

    Chiuchiungkeng fault ?

  • Chungcheng unisersity

    Uplift (cm)

    Strike slip (cm)

  • 1906: Meishan fault

  • 1906:Meishan fault

  • 1906:Meishan fault

  • 嘉義廳(嘉義市內)前大馬路二側潰倒的民宅與散落一地的殘磚礫瓦。

  • 嘉義廳大莆林街(嘉義縣大林鎮)的慘狀,擔架是當時運送傷患的主要工具。大莆林街民房全倒124戶、半倒12戶、大破10戶,35人死亡、10人重傷、24人輕傷。

  • Chung-Cheng Unisersity

  • Yui et al.,2003

  • Muchiliao active structure

  • Complex faulting process

    Chiayi transfer structure

  • South ending process of the 1999 Chi-Chi earthquake

  • 1022 Mw 6.8earthquake

    No surface rupture

    1999 Chi-Chi earthquake

    S N

    2.4m

    Complex ending process rather than a single tear fault

  • Kukeng fault

    Changhua fault

    Chiuhsiungkeng fault

    1. Kukeng fault & Changhua fault

    2. Kukeng fault & Chiuchiungkeng fault

    2. Chiai blind fault & Meishan fault

    Chiayi blind thrust

    Meishan fault

    Chenglongpu faultWhat is the return period of each fault?

    Earthquake hazard assessment?

  • Cut 18540yr terrace(Hsu ,2003)Vertical displacement > 0.72 mm/yrHorizontal displacement > 15 mm/yr

    Chiuchiungkeng fault

  • 區域地形

  • Chiayi blind fault

    Meishan fault

    Chiayi blind fault

    High angle dipping to the south

  • Meishan Fault

    Meishan Fault

    Chiuchiungkeng FaultMeishan Fault

    (Cheng, 1995)

    Yang et al.,2004

  • Meishan Fault

    Meishan Fault

    Chiuchiungkeng FaultMeishan Fault

    (Cheng, 1995)

  • (Cheng, 1995)

  • Structure of Cretaceous TopTaihsi

    Touliu

    Tounan

    Meishan

    PeikangMinhsiung

    AnticlineSyncline

    Meishan Fault

  • Meishan Fault

    Chiuchiungkeng FaultMeishan Fault

    (Cheng, 1995)Blind fault beneath the Chiungekeng fault

  • Meishan Fault

    Blind fault beneath the Chiuchiungkeng Fault

  • ure of Cretaceous Top TouliuTounan

    Meishan

    eikangMinhsiung

  • Yang et al.,2004

  • Kukeng fault →strike slip fault : >20 Km

    Meishan fault →strike slip fault: ~25 km

    Chiuchiungkeng fault→ thrust fault → >17 Km

    Chiayi fault →blind thrust→ > 30 Km

    Liuchia fault → blind thrust → > 20 km

    Muchiliao fault → blind thrust → 24 Km

    Peiho fault→strike slip fault→ >13 Km

    Chung Cheng University

  • 1.Thickness of the sedimentary basin

    2.Preexisting structures

    3.Changing the lithology

    Basin is deeper to the south

  • Lin et a.,2002

    South dipping faults are easy to be triggered

  • Thank you for your attention