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    Tectonic implications of uplifted Holocene marine terracesTectonic implications of uplifted Holocene marine terracesinin PangasinanPangasinan and Davao Oriental, Philippinesand Davao Oriental, Philippines

    NoelynnaNoelynna T.T. RamosRamosaa, Hiroyuki, Hiroyuki TsutsumiTsutsumibb, Jeffrey S., Jeffrey S. PerezPerezb,cb,c, and Percival P., and Percival P. BermasBermas,, Jr.Jr.dd

    aaRushurgentRushurgent Working Group, National Institute of Geological Sciences, College of Science,Working Group, National Institute of Geological Sciences, College of Science,

    University of the Philippines,University of the Philippines, DilimanDiliman, Quezon City 1101, Philippines, Quezon City 1101, PhilippinesbbDepartmentDepartment of Geophysics, Graduate School of Science, Kyoto University, Kyoto 606of Geophysics, Graduate School of Science, Kyoto University, Kyoto 606--8502, Japan8502, Japan

    ccDepartmentDepartment of Science and Technologyof Science and Technology -- Philippine Institute ofPhilippine Institute of VolcanologyVolcanology and Seismology,and Seismology,

    C. P. Garcia Avenue,C. P. Garcia Avenue, DilimanDiliman, Quezon City 1104, Philippines, Quezon City 1104, PhilippinesddMinesMines and Geosciences Bureau XIand Geosciences Bureau XI -- Department of Environment and Natural Resources,Department of Environment and Natural Resources,

    6969 KonsuelaKonsuela Bldg., cor. Jacinto St., Davao City 8000, PhilippinesBldg., cor. Jacinto St., Davao City 8000, Philippines

    GeoConGeoCon 2011: Geology Working For A Resilient Society2011: Geology Working For A Resilient Society

    CrowneCrowne Plaza Hotel, Quezon CityPlaza Hotel, Quezon City

    08 December 201108 December 2011

    NoelynnaNoelynna T.T. RamosRamosaa, Hiroyuki, Hiroyuki TsutsumiTsutsumibb, Jeffrey S., Jeffrey S. PerezPerezb,cb,c, and Percival P., and Percival P. BermasBermas,, Jr.Jr.dd

    aaRushurgentRushurgent Working Group, National Institute of Geological Sciences, College of Science,Working Group, National Institute of Geological Sciences, College of Science,

    University of the Philippines,University of the Philippines, DilimanDiliman, Quezon City 1101, Philippines, Quezon City 1101, PhilippinesbbDepartmentDepartment of Geophysics, Graduate School of Science, Kyoto University, Kyoto 606of Geophysics, Graduate School of Science, Kyoto University, Kyoto 606--8502, Japan8502, Japan

    ccDepartmentDepartment of Science and Technologyof Science and Technology -- Philippine Institute ofPhilippine Institute of VolcanologyVolcanology and Seismology,and Seismology,

    C. P. Garcia Avenue,C. P. Garcia Avenue, DilimanDiliman, Quezon City 1104, Philippines, Quezon City 1104, PhilippinesddMinesMines and Geosciences Bureau XIand Geosciences Bureau XI -- Department of Environment and Natural Resources,Department of Environment and Natural Resources,

    6969 KonsuelaKonsuela Bldg., cor. Jacinto St., Davao City 8000, PhilippinesBldg., cor. Jacinto St., Davao City 8000, Philippines

    GeoConGeoCon 2011: Geology Working For A Resilient Society2011: Geology Working For A Resilient Society

    CrowneCrowne Plaza Hotel, Quezon CityPlaza Hotel, Quezon City

    08 December 201108 December 2011

    Holocene coastal uplift in the western PacificHolocene coastal uplift in the western Pacific

    HT: 6 (21 m)

    HT: 6 (11 m)

    HT: 7 (24 m)

    (80 m)

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    Bathymetriy: NGDC; Topography: SRTM; PFZ: Tsutsumi and Perez, 2010; Instrumental seismicity (M>6) (1897-2008): PHIVOLCS;

    Historical seismicity (M>6) (1619-1894): Bautista and Oike, 2000

    1897 - 2008 1619 - 1894

    Seismicity in the PhilippinesSeismicity in the Philippines

    Holocene coastal uplift in the western PacificHolocene coastal uplift in the western Pacific

    HT: 6 (21 m)

    HT: 6 (11 m)

    HT: 7 (24 m)

    (80 m)

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    ObjectivesObjectives

    To identify and systematically map Holocene marine

    terraces in Pangasinan and Davao Oriental

    To evaluate the seismotectonic potential of tectonic

    structures (e.g. Manila trench, Philippine trench)

    Western PangasinanWestern Pangasinan

    Bathymetry: NGDC; Topography: NASA; GPS vectors: Rangin et al., 1999; Focal mechanisms (1976-2008): Global CMT;

    Seismicity (1897-2008) and PFZ: PHIVOLCS

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    Terrace mapsTerrace maps

    Modified from Maemoku and Paladio, 1992

    Holocene marine terracesHolocene marine terraces

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    Holocene marine terracesHolocene marine terraces

    Deformation pattern and tectonic implicationsDeformation pattern and tectonic implications

    prehistoric earthquakes are

    probably offshore

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    Elastic dislocation model 1: Megathrust faultElastic dislocation model 1: Megathrust fault

    Fault parametersFault model

    b-b c-c

    Strike () 0 N-S N-S

    Dip angle () 30~50 30 40

    Top depth (km) 0 0 0

    Bottom depth (km) 40~70 50 60

    Amount of reverseslip (m) 10~26 16 16

    Fault parametersFault model

    b-b c-c

    Strike () 0 N-S N-S

    Dip angle () 30~50 30 40

    Top depth (km) 0 0 0

    Bottom depth (km) 40~70 50 60

    Amount of reverseslip (m) 10~26 16 16

    Elastic dislocation model 1: Megathrust faultElastic dislocation model 1: Megathrust fault

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    Fault parametersFault model

    a-a c-c

    Strike () 0 N-S N-S

    Dip angle () 30~80 30 60

    Top depth (km) 0 0 0

    Bottom depth (km) 15~40 15 30

    Amount of reverseslip (m) 7~9 9 7

    Elastic dislocation model 2: Intraplate faultElastic dislocation model 2: Intraplate fault

    Fault parametersFault model

    a-a c-c

    Strike () 0 N-S N-S

    Dip angle () 30~80 30 60

    Top depth (km) 0 0 0

    Bottom depth (km) 15~40 15 30

    Amount of reverseslip (m) 7~9 9 7

    Elastic dislocation model 2: Intraplate faultElastic dislocation model 2: Intraplate fault

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    Eastern Davao OrientalEastern Davao Oriental

    Bathymetry: NGDC; Topography: NASA; GPS vectors: Rangin et al., 1999; Focal mechanisms (1976-2008): Global CMT;

    Seismicity (1897-2008): PHIVOLCS; PFZ main trace: Tsutsumi and Perez (2010)

    Holocene marine terracesHolocene marine terraces

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    Deformation patternDeformation pattern

    ConclusionsConclusions

    Pangasinan

    Davao Oriental

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    Summary and conclusionsSummary and conclusions

    Pangasinan Davao Oriental

    Elevation of

    paleoshoreline

    angle (m amsl)

    TIV -- 8~12TIII / T3 4~11 6~10

    TII / T2 2~7 3~6

    TI / T1 1~5 1~5

    Radiocarbon

    ages (cal yr BP)6480 to 1325 8080 to 4140

    Maximum uplift

    rate (mm/yr)

    Pleistocene ~1.3 ~1.3

    Holocene ~1.7 ~1.5

    Deformation

    pattern

    paleoshoreline angles are highest along headlands

    facing the subduction zone (e.g. Manila trench,

    Philippine trench)Uplift

    mechanismcoseismic uplift

    Earthquake

    magnitude7.7~8.5 > 7.5

    Source fault offshore reverse fault (offshore reverse fault)

    Thank youThank you

    Kyoto University (Active Tectonics lab, S. Toda, N.Kyoto University (Active Tectonics lab, S. Toda, N. ShimobayashiShimobayashi))

    PaleoLabPaleoLab, Japan, Japan

    Y. Ota, A.Y. Ota, A. MeltznerMeltzner, M. Liu,, M. Liu, J.B.H.ShyuJ.B.H.Shyu, N. Litchfield, N. Litchfield

    University of the Philippines (University of the Philippines (RushurgentRushurgent Working GroupWorking Group -- NationalNational

    Institute of Geological Sciences, Marine Science Institute)Institute of Geological Sciences, Marine Science Institute)

    Philippine Institute of Volcanology and SeismologyPhilippine Institute of Volcanology and Seismology

    Mines and Geosciences BureauMines and Geosciences Bureau

    local government officials oflocal government officials of PangasinanPangasinan and Davao Orientaland Davao Oriental

    provincesprovinces