Archaeoseismology and Palaeoseismology in the Alpine ... - Tierra

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1 st INQUA‐IGCP‐567 International Workshop on Earthquake Archaeology and Palaeoseismology Koster, A., Vonberg, D. and Reicherter, K. Tsunamigetic deposits along the southern Gulf of Cádiz (southwestern Spain) caused by tsunami in 1755?................................................................................................................................... 73 Kostov, K., Shanov, S. and Surányi, G. Palaeoseismological investigations using speleothems: case study of two caves in Rhodopes Mountains, Southern Bulgaria................................................................................................... 76 Lee, M., Han, S.R., Shim, T. and Kim, Y.S. Characteristics and paleoseismic study of the Quaternary Eupcheon fault in Southeast Korea................................................................................................................................................... 79 Maestro, A., Jané, G., García-Mayordomo, J., Fernández-Revuelta, B., Rodríguez-Pascua, M.A. and Martínez-Díaz, J.J. Paleoseismic evidence from broken submarine carbonate chimneys in the Gulf of Cádiz (Southern Spain)................................................................................................................................... 83 Michetti, A.M., Vittori, E., Berlusconi, A., Blumetti, A.M., Comerci, V., Di Manna, P., Esposito, E., Guerrieri, L., Livio, F., Porfido, S. and Sileo, G. Earthquake ground effects during moderate events: the l’Aquila 2009 event case history ............................... 87 Moreno, X., Gràcia, E., Masana, E., Rodés, Á., Bartolomé, R. and Pallàs, R. Paleoseismology along the Carboneras Fault: integrated onshore-offshore evidence of seismogenic activity............................................................................................................................... 91 Mörner, N.A. Liquefaction as evidence of paleoseismics................................................................................................. 95 Ortuño, M. Criteria to distinguish neotectonic from other active faults: examples from the Central Pyrenees .............................................................................................................................................. 98 Papanikolaou, I.D. The ESI 2007, the intensity attenuation relationships and possible gains for seismic hazard maps....................................................................................................................................... 102 Papathanassiou, G. and Pavlides, S. Gis-Based database of earthquake-induced liquefaction manifestations in Broader Aegean Region, DALO v.1.0 ................................................................................................................. 106 Rodríguez-Pascua, M.A., Abad Casal, L., Pérez-López, R., Gamo Parra, B., Silva, P.G., Garduño-Monroy, V.H., Giner-Robles, J.L., Israde-Alcántara, I., Bischoff, J. and Calvo, J.P. Roman, visigoth and islamic evidence of earthquakes recorded in the archaeological dite of El Tolmo de Minateda (Prebetic Zone, Southeast of Spain) ................................................................... 110 Rodríguez-Pascua, M.A., Pérez-López, R., Giner-Robles, J.L., Silva P.G., Garduño- Monroy, V.H. and Reicherter, K. A comprehensive classification of Earthquake Archaeological Effects (EAE) for structural strain analysis in archaeoseismology...................................................................................................... 114 Rodríguez-Peces, M.J., García-Mayordomo, J., Azañón, J.M., Insua-Arévalo, J.M. and Jiménez Pintor, J. Preliminary results of static and dynamic reconstruction of Güevéjar landslide (Granada, Spain) during 1775 Lisbon and 1884 Andalusian earthquakes ................................................................... 118 Rodríguez-Vidal, J., Cáceres, L.M., Ruiz, F., Abad, M., Fa, D., Finlayson, G., Finlayson, J.C. and Bailey, G. Geomarkers of AD 1755 Tsunami on Gibraltar......................................................................................... 122 Samari, H. and Mobini, A. The important key factor of paleotectonic studies on seismic hazard evaluation of Moshampa dam and hydropower plant ................................................................................................... 125 Sánchez-Gómez, M., Martínez-Sánchez, C., García-García, F., Peláez, J.A., Pérez-Valera, F. and Martínez-Andreu, M. Evidence for a holocene earthquake recorded in a fluvial-archaeological sequence of the Segura river, SE Spain ......................................................................................................................... 129 Schaub, A., Reicherter, K., Grützner, C. and Fernández-Steeger, T. Evidence for a medieval earthquake in the Aachen area (Germany), revealed by structural damage in the cathedral ........................................................................................................ 132 178
1 st INQUA‐IGCP‐567 International Workshop on Earthquake Archaeology and Palaeoseismology Schreiber, S., Hinzen, K.G. and Fleischer, C. An application of 3D laser scanning in archaeology and archaeoseismology: the Medieval Cesspit in the Archaeological Zone Cologne, Germany .............................................................................. 136 Silva, P.G., Rodríguez Pascua, M.A., Pérez López, R., Giner-Robles, J.L., Lario, J.; Bardají, T., Goy, J.L. and Zazo, C. Geological and archaeological record of the 1504 AD Carmona earthquake (Guadalquivir Basin, South Spain): a review after Bonsor, 1918.................................................................................... 139 Sintubin, M., Stewart, I.S., Niemi, T. and Altunel, E. Archaeoseismology: past, present and future .......................................................................................... 143 Stančikaitė, M., Kisielienė, D., Mažeika, J., Guobytė, R. and Blaževičius, P. Geological-geomorphological setting and human interference during the 13th-15th centuries AD at Vilnius Lower Castle, East Lithuania................................................................................. 146 Štěpančíková, P., Hók, J. and Nývlt, D. Trenching survey on the south-eastern section of the Sudetic Marginal Fault (NE Bohemian massif, intraplate region of Central Europe) ............................................................................. 150 Tahir Mian, M. Geomorphology, paleoseismology and geological analysis for seismic hazard estimations ............................. 152 Tatevossian, R.E. Geological and macroseismic effects of Muya, 1957, earthquake and paleoearthquakes in Baikal region, Russia............................................................................................................................ 156 Villa Valdés, A. Geoarchaeological context of the destruction and abandonment of a fortified village in Asturias in the 2nd century AD: Chao Samartín (Grandas de Salime, Asturias, Spain) .................................. 160 Vollmert, A., Reicherter, K. and Grützner, C. The origin of rockfalls and the formation of hanging valleys along the La Laja range front (Tarifa, S. Spain)................................................................................................................................. 162 Vött, A., Bareth, G., Brückner, H., Fountoulis, I., Lang, F., Kelletat, D., Sakellariou, D., Scheffers, A. and Scheffers, S. Palaeotsunami signatures in Holocene coastal geo-archives of the eastern Ionian Sea region, Greece .................................................................................................................................... 165 Wiatr, T., Reicherter, K. and Papanikolaou, I. Terrestrial laser scanning of an active fault in Greece: Kaparelli Fault......................................................... 169 Yerli , B., Schreiber, S., Hinzen, K.G., ten Veen, J.H. and Sintubin, M. Testing the hypothesis of earthquake-related damage in structures in the lycian ancient city of Pinara, SW Turkey ..................................................................................................................... 173 179
Page 1:
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 131 and 132: 1 st INQUA‐IGCP‐567 Internation
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 and 178: (~40 cm), F‐ rotated building str
Page 179: Index 1 st INQUA‐IGCP‐567 Inter
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