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Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US.

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Presentation on theme: "Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US."— Presentation transcript:

1 Pelatihan : Techniques in Active Tectonic Study Juni 20-Juli 2, 2013 Instruktur: Prof. J Ramon Arrowsmith (JRA) Dari Arizona State University (ASU) - US Tempat Pelaksanaan: Ruang Pangea, Laboratorium Gempabumi (LabEarth) – Puslit Geoteknologi LIPI dan Kuliah lapangan akan dilakukan disekitar Sesar Lembang, Jawa Barat. * Lebih jelas baca TOR/KAK dan daftar acara

2 Subduction I: Japan 2011 earthquake Outline of this lecture Seismicity Seismic waves Displacements on land and seafloor Source models Seismic coupling Comparison with other events

3 March 11, 2011 Tohoku, Japan M9.0 Earthquake http://www.nature.com/ngeo/journal/v1/n11/fig_tab/ngeo341_F1.html

4

5 Magnitude 9.0 NEAR THE EAST COAST OF HONSHU, JAPAN Friday, March 11, 2011 at 05:46:23 UTC Japan was struck by a magnitude 9.0 earthquake off its northeastern coast Friday March 11, 2011. This is one of the largest earthquakes that Japan has ever experienced.. USGS Part of houses swallowed by tsunami burn in Sendai, Miyagi Prefecture (state) after Japan was struck by a strong earthquake off its northeastern coast Friday, March 11, 2011. New York Times In downtown Tokyo, large buildings shook violently and there was severe flooding due to a tsunami generated by the earthquake.

6 Tsunami waves swept away houses and cars in northern Japan and pushed ships aground. The tsunami waves traveled far inland, the wave of debris racing across the farmland, carrying boats and houses with it. Houses were washed away by tsunami in Sendai, Miyagi Prefecture in eastern Japan, after Japan was struck by a magnitude 9.0 earthquake off the northeastern coast. New York Times Magnitude 9.0 NEAR THE EAST COAST OF HONSHU, JAPAN Friday, March 11, 2011 at 05:46:23 UTC The tsunami, seen crashing into homes in Natori, Miyagi prefecture. AP

7 March 25, 2011 estimates: 10,066 people confirmed dead and 17,443 people are reported missing >$300B economic losses

8 Seismicity of northern Japan since 1973 http://eqseis.geosc.psu.edu/~cammon/Japan2011EQ/

9 Foreshocks, Mainshock, Aftershocks Movie 2.5

10 Japan 2011 Aftershocks http://eqseis.geosc.psu.edu/~cammon/Japan2011EQ/

11 Tohoku, Japan Earthquake: Aftershock (and Foreshock) Sequence, 03/08/11 - 03/16/11

12 Tohoku, Japan Earthquake: Aftershock (and Foreshock) Sequence, M:Time History

13 Simple view of the seismic wave propagation http://www.iris.edu/hq/retm/#1328http://www.iris.edu/hq/retm/#1328;

14 Simple view of the seismic wave propagation http://www.iris.edu/hq/retm/#1328http://www.iris.edu/hq/retm/#1328;

15 Seismic wave propagation http://www.iris.edu/hq/retm/#1328http://www.iris.edu/hq/retm/#1328;

16 Seismic wave propagation http://www.iris.edu/hq/retm/#1328http://www.iris.edu/hq/retm/#1328;

17 Tohoku, Japan Earthquake: Shaking Duration in Tokyo, Ground Acceleration 1g = 9.8e+002 gal +/-17%g

18 6 minutes Tohoku, Japan Earthquake: Shaking Duration in Tokyo, Ground Velocity

19 Videos from Tokyo and nearby http://www.youtube.com/watch?v=oQVPfQu 50yY –EEW works! http://www.youtube.com/watch?v=oQVPfQu 50yY http://www.youtube.com/watch?v=dN4NBK1 veb0 –train stopped http://www.youtube.com/watch?v=dN4NBK1 veb0 http://www.youtube.com/watch?v=64PEo29h BGY –Tokyo skyscrapers swaying http://www.youtube.com/watch?v=64PEo29h BGY http://tremblingearth.wordpress.com/2011/03 /13/more-unique-perspectives-of-the-8-9- quake/

20 Tohoku, Japan Earthquake: Finite Fault Model USGS V1 - 7 hrs after OT Compact rupture, mostly bilateral about epicenter, peak slip up dip of hypocenter. Rupture was likely restricted to the shallow trench, and GPS vectors suggest slip did not reach the plate boundary beneath the coastline. Peak slips closer to 40+ m, inferred from updated modeling. Box is 580 km long and 190 km wide Zone of main slip is 300 km long and ~150 wide M 0 = mu*A*u_bar -mu = 30 GPa (3x10 10 N/m 2 ) -A is surface area that slipped (m 2 ) [width x length] -u_bar is the average slip in meters japan = mu.*500.*km.*200.*km.*11 = 3.3000e+022 Nm japan_mw=(2./3).*log10(japan)-6 = 9.0123

21 M Simons et al. Science 2011;332:1421-1425

22 Evolving displacement field http://gps.alaska.edu/ronni/sendai2011.html

23 acquired February 26, 2011 http://earthobservatory.nasa.gov/NaturalHazards/view.php?id=49630

24 Coastal inundation and permanent subsidence (?) acquired March 12, 2011

25 http://www1.kaiho.mlit.go.jp/e/KAIYO/image/Seafloor_Geodetic_Observation.gif

26 Sato, et al., 2011

27 M Simons et al. Science 2011;332:1421-1425

28 USArray http://www.tectonics.caltech.edu/slip_history/2011_taiheiyo-oki/Backprojection/ Dense Euro Backprojection of seismic energy to source

29 Ide, et al., 2011

30 Coulomb calculation

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32 Lay and Kanamori, 2011

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34 Ando and Imanishi, 2011 Foreshock-Mainshock linkage

35 Lay and Kanamori, 2011

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37 Japanese subduction zone segmentation and hazard assessment: Expectation was for individual patches to rupture (M~8—consistent with historic behavior). Tsunami hazard was based on last few centuries record. http://www.jishin.go.jp/main/chousa/10_yosokuchizu/k_j ishincategory.pdfhttp://www.jishin.go.jp/main/chousa/10_yosokuchizu/k_j ishincategory.pdf modified: http://home.hiroshima- u.ac.jp/kojiok/110311EQ/HERPmapwithnotes1.pdfhttp://home.hiroshima- u.ac.jp/kojiok/110311EQ/HERPmapwithnotes1.pdf

38 Subduction I: Japan 2011 earthquake Outline of this lecture Seismicity Seismic waves Displacements on land and seafloor Source models Seismic coupling Comparison with other events


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