Archaeoseismology and Palaeoseismology in the Alpine ... - Tierra

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Ambraseys, N.N., Smit, P., Douglas, J., Margaris, B., Sigbjörnsson, R., Ólafsson, S., Suhadolc, P., Costa, G. (2004). Internet site for strong‐motion data. Boll. Geof. Teor. Appl., 45, n. 3, 113‐129. Armijo, R., Meyer, B., Hubert, A., Barka, A. (1999). Westward propagation of the North Anatolian fault into the northern Aegean: timing and kinematics. Geology, 27 (3), 267–270. Barka, A. and Reilinger R. (1997). Active Tectonics of Eastern Mediterranean region: deduced from GPS, neotectonic and seismicity data. Annali Di Geofisica, 40, n. 3, 587‐610. Barka, A., and Kandinsky‐Cade, K. (1988). Strike‐slip fault geometry in Turkey and its influence on earthquake activity. Tectonics, 7 (3), p. 663–684. Collins, A.S., and Robertson, A.H.F. (1999). Evolution of the Lycian Allochthon, western Turkey, as a north‐facing Late Palaeozoic to Mesozoic rift and passive continental margin. Geol. J., 34, 107–138. Guidoboni, E. (1994). Catalogue of ancient earthquakes in the Mediterranean area up to the 10 th century. Rome, Istituto Nazionale di Geofisica, 504 p. Guidoboni, E. (2002). Historical seismology: the long memory of the inhabited world, in: International Handbook of Earthquake and Engineering Seismology. W. H. K. Lee, Kanamori H., Jennings P. C., and Kisslinger C., (Eds.) International Geophysics Series, 81A, Academic Press, Amsterdam, p. 775– 790. Hinzen, K.‐G. (2005). The use of engineering seismological models to interpret archaeoseismological findings in Tolbiacum, Germany: a case study. Bull. Seism. Soc. Am., 95 (2), 521–539. Kamai, R., and Hatzor, Y.H. In press. Numerical analysis of block displacements in ancient masonry structures: a new method to estimate historic ground motions. International Journal for Numerical and Analytical Methods in Geomechanics. doi:10.1002/nag.671. 1 st INQUA‐IGCP‐567 International Workshop on Earthquake Archaeology and Palaeoseismology 176 Lang, G. (2003). Klassische antike Stätten Anatoliens, Band II. Lang Verlag, St. Peter am Hart, 707 p. Marco, S. (2008). Recognition of earthquake‐related damage in archaeological sites: Examples from the Dead Sea fault zone. Tectonophysics 453, 148‐156. Sintubin, M., Stewart, I. (2008). A Logical Methodology for Archaeoseismology: A Proof of Concept at the Archaeological Site of Sagalassos, Southwest Turkey. Bulletin of the Seismological Society of America, 98(5), 2209‐2230; DOI: 10.1785/0120070178. Soysal, H., Sipahioğlu, S., Kolçak, D., and Altınok, Y. (1981). Historical Earthquake Catalogue of Turkey and Surrounding Area (2100 B.C. – 1900 A.D.). Technical Report, TUBITAK, no. TBAG‐341. ten Veen, J.H. (2004). Extension of Hellenic forearc shear zones in SW Turkey: the Pliocene–Quaternary deformation of the Eşen Çay Basin. Journal of Geodynamics, 37, 181–204. ten Veen, J.H., Boulton, S. and Alçiçek, M.C. (2008). From palaeotectonics to neotectonics in the Neotethys realm: The importance of kinematic decoupling and inherited structural grain in SW Anatolia (Turkey). Tectonophysics, doi: 10.1016/j.tecto.2008.09. 030 (in press). Westaway, R. (1994). Present‐day kinematics of the Middle and Eastern Mediterranean. J. Geophys. Res., 99, 20203–20223. Wurster, W., Wörrle, M. (1978). Die Stadt Pinara. Deutsches Archaeologisches Intitut, Archaeologischer Anzeiger 1978 Heft 1, 74‐99 Yerli, B., ten Veen, J.H., Sintubin, M., Karabacak, V., Yalciner, C., Altunel, E. Submitted. Assessment of seismically induced damage using LIDAR: the ancient city of Pınara (SW Turkey) as a case study. Geological Society of America Special Paper Ancient Earthquakes.
Index 1 st INQUA‐IGCP‐567 International Workshop on Earthquake Archaeology and Palaeoseismology Azañón, J.M., García-Mayordomo, J., Insua-Arévalo, J.M. and Rodríguez-Peces, M.J. Paleosismological features of the Granada fault ......................................................................................... 5 Besana-Ostman, G.M., Ando, M and Fonseca, J.F. Ground rupture induced by 2003 Masbate earthquake, Philippines ................................................................ 8 Bjerrum, L.W., Sørensen, M.B. and Atakan, K. Simulated ground motions of the May 12 2008, Wenchuan (China) earthquake – comparison with damage distribution ....................................................................................................... 12 Braun, Y., Bar-Matthews, M., Ayalon, A., Kagan, E. and Agnon, A. Dating paleo-seismic activity on the Carmel Fault during the Quaternary, Mt. Carmel, Israel ................................................................................................................................................... 16 Chatzipetros. A. and Pavlides, S. A rare case of preserved earthquake ruptures in an archaeological site: Mikri Doxipara – Zoni, NE Greece .................................................................................................................................... 20 Da-Quan, Y., Zhi, S., Xiao-Gi, S. , Jie-Ping, T. and An-Guo, C. Discovery of natural deformation relics in Anhui archaeological area and its significance................................. 23 Ferry, M., Meghraoui, M., Abou Karaki, N. and Al-Taj, M. Earthquake clustering along the Dead Sea Fault (Jordan) from geomorphology, palaeoseismology and archaeoseismology................................................................................................. 26 García-Mayordomo, J., Rodríguez Peces, M.J., Azañón, J.M and Insua-Arévalo, J.M. Advances and trends on earthquake-triggered landslide research in Spain .................................................... 28 Gath, E.M. and Rockwell, T.K. Coseismic offset of the Camino de Cruces confirms the Pedro Miguel fault as the cause of the AD 1621 Panamá Viejo Earthquake .................................................................................................... 32 Grützner, C. and Reicherter, K. The Baelo Claudia earthquake problem approached with semi-quantitative logic trees.................................... 35 Guerrieri, L., Porfido, S., Esposito, E., Blumetti, A.M., Michetti, A.M. and Vittori, E. Cataloguing earthquake environmental effects: a tool for the comparison of recent, historical and paleo-earthquakes ............................................................................................................. 39 Gutiérrez, F. Lucha, P. and Jordá, L. The Río Grío Depression (Iberian Range, NE Spain). Neotectonic graben vs. fluvial valley ............................... 43 Hinzen, K.G. Dynamic response of simple structures..................................................................................................... 47 Hinzen, K.G., Fleischer, C., Reamer, S.K., Schreiber, S., Schütte, S. and Yerli, B. Quantitative methods in archaeoseismology.............................................................................................. 50 Höbig, N., Brau, A., Grützner, C., Fernández-Steeger, T. and Reicherter, K. Rock fall hazard mapping and run out simulation: a case study from Bolonia Bay, southern Spain...................................................................................................................................... 52 Hoffmann, N., Reicherter, K., Grützner, C., Wiatr, T. and T. Fernández-Steeger Tectonic morphology of the Lake Ohrid basin (Fyrom, Allbania) ................................................................... 56 Insua-Arévalo, J.M. and García-Mayordomo, J. Upper Pleistocene tectonic activity in the Central Pyrenees Range (Navarra, N Spain) .................................... 60 Jin, K., Lee, M. and Kim, Y.S. Archaeoseismological approach on stone heritages in Gyeongju Area, SE Korea ............................................ 63 Kamai, T. and Sangawa, A. Landslides on ancient fill structures induced by the 16 th century earthquake in the Kinki district, Japan ....................................................................................................................................... 67 Kanari, M., Katz, O., Porat, N., Weinberger, R. and Marco, S. Evaluation of rockfall hazard to the town of Qiryat Shemona, N. Israel. Possible correlation to Earthquakes ...................................................................................................................... 70 177
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Abstracts Volume Archaeoseismology
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Edita e imprime: Sección de Public
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1 st INQUA‐IGCP‐567 Internation
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the importance of performing absolu
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indicative of strike‐slip faultin
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DISCUSSION Based on detailed field
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Table 1: Source parameters used in
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elations. However, the attenuation
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mostly concentrated on the DST in I
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continuous support. N. Shalev, G. G
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The tumulus initial morphology show
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our understanding and prediction of
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spans, with a threefold increase fr
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Nevertheless the lack of research,
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earthquake. In uncertain cases, as
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The site reconnaissance successfull
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Table 1: Surface faulting extent re
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The graben has a markedly asymmetri
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are a valuable addition to the rout
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to 400 m) the calculated values for
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RISK ANALYSIS The created hazard ma
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290 m water depth the basin accumul
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CONCLUSIONS From the palaeostress a
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Fig. 2: Geological map of the study
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however, the massive 1995 earthquak
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mapped on the slopes above Qiryat
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interpreted as either an expression
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The Shepran Cave is located on the
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properties. The mean value of speci
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excavated a deep trench, thus provi
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Fig. 8: Seismic ground shaking may
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elevant qualitative criteria are po
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CONCLUDING REMARKS The exposed exam
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produced by significantly different
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It is possible that a portion of th
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In addition, the Database of histor
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were published by IGME (1983) and E
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The city collapsed and it was aband
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Fig. 4: Slipped lintel in a window
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to overcome shear resistance and in
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Newmark, N.M. (1965). Effects of ea
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associated with various tsunamis (<
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Page 129 and 130: this method, the magnitude of the e
Page 133 and 134: etween pieces. Fragments have not f
Page 137 and 138: on the exact date of the earthquake
Page 139 and 140: THE ARCHAEOLOGICAL ZONE COLOGNE Aft
Page 143 and 144: affecting the Alcázar was about 50
Page 147 and 148: archaeoseismology could instead bec
Page 149 and 150: In the area later occupied by Vilni
Page 155 and 156: Fig. 2: Assemblage of landforms ass
Page 157 and 158: Fig. 8: Data and regression for mag
Page 159 and 160: Fig. 3: Relationships among magnitu
Page 161 and 162: CONCLUSIONS 1. Spatial distribution
Page 163 and 164: The stratigraphic sequence (Fig. 4)
Page 165 and 166: especially in the zones of hanging
Page 169 and 170: interpretations are based on relati
Page 173 and 174: Fig. 5: Gray‐scale value laser im
Page 177: (~40 cm), F‐ rotated building str
Page 181: 1 st INQUA‐IGCP‐567 Internation
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