Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/12208| DC Field | Value | Language |
|---|---|---|
| dc.date.accessioned | 2019-02-01T08:20:48Z | en |
| dc.date.available | 2019-02-01T08:20:48Z | en |
| dc.date.issued | 2018 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/12208 | en |
| dc.description | This article has been accepted for publication in Geophysical Journal International ©: The Authors 2018. Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved. Uploaded in accordance with the publisher's self-archiving policy. | en |
| dc.description.abstract | We present an improved picture of the ongoing crustal deformation field for the Zagros Fold-and-Thrust Belt continental collision zone by using an extensive combination of both novel and published GPS observations. The main results define the significant amount of oblique Arabia–Eurasia convergence currently being absorbed within the Zagros: right-lateral shear along the NW trending Main Recent fault in NW Zagros and accommodated between fold-and-thrust structures and NS right-lateral strike-slip faults on Southern Zagros. In addition, taking into account the 1909–2016 instrumental seismic catalogue, we provide a statistical evaluation of the seismic/geodetic deformation-rate ratio for the area. On Northern Zagros and on the Turkish–Iranian Plateau, a moderate to large fraction (∼49 and >60 per cent, respectively) of the crustal deformation occurs seismically. On the Sanandaj–Sirjan zone, the seismic/geodetic deformation-rate ratio suggests that a small to moderate fraction (<40 per cent) of crustal deformation occurs seismically; locally, the occurrence of large historic earthquakes (M ≥ 6) coupled with the high geodetic deformation, could indicate overdue M ≥ 6 earthquakes. On Southern Zagros, aseismic strain dominates crustal deformation (the ratio ranges in the 15–33 per cent interval). Such aseismic deformation is probably related to the presence of the weak evaporitic Hormuz Formation which allows the occurrence of large aseismic motion on both subhorizontal faults and surfaces of décollement. These results, framed into the seismotectonic framework of the investigated region, confirm that the fold-and-thrust-dominated deformation is driven by buoyancy forces; by contrast, the shear-dominated deformation is primary driven by plate stresses. | en |
| dc.language.iso | English | en |
| dc.publisher.name | Oxford University Press on behalf of The Royal Astronomical Society | en |
| dc.relation.ispartof | Geophysical Journal International | en |
| dc.relation.ispartofseries | /213 (2018) | en |
| dc.subject | Creep and deformation | en |
| dc.subject | Satellite geodesy | en |
| dc.subject | Asia | en |
| dc.subject | Earthquake hazards | en |
| dc.subject | Seismicity and tectonics | en |
| dc.title | An improved evaluation of the seismic/geodetic deformation-rate ratio for the Zagros Fold-and-Thrust collisional belt | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | 194-209 | en |
| dc.identifier.URL | https://academic.oup.com/gji/article/213/1/194/4712013 | en |
| dc.subject.INGV | Geodynamics and Tectonics | en |
| dc.identifier.doi | 10.1093/gji/ggx524 | en |
| dc.relation.references | Alipoor, R., Zaré, M. & Ghassemi, M.R., 2012. Inception of activity and slip rate on the Main Recent Fault of Zagros Mountains, Iran, Geomorphology, 175-176, 86-97, doi:10.1016/j.geomorph.2012.06.025. Allen, M.B., Saville, C., Blanc, E.J.-P., Talebian, M. & Nissen, E., 2013. Orogenic plateau growth: Expansion of the Turkish-Iranian Plateau across the Zagros fold-and-thrust belt, Tectonics, 32, 171-190, doi:10.1002/tect.20025. Ambraseys, N.N. & Jackson, J.A., 1998. Faulting associated with historical and recent earthquakes in the Eastern Mediterranean region, Geophys. J. Int., 133, 390-406, doi:10.1046/j.1365-246X.1998.00508.x. Ambraseys, N.N. & Melville, C., 1982. A History of Persian Earthquakes, Cambridge University Press, Cambridge. Ambraseys, N.N., 1989. Temporary seismic quiescence: SE Turkey, Geophys. J. Int., 96 (2), 311-331, doi:10.1111/j.1365-246X.1989.tb04453.x. Ansari, S. & Zamari, A., 2014. Short-term seismic crustal deformation of Iran, Ann. Geophys., 57 (2), S0210, doi:10.4401/ag-6413. Aqrawi, A.A.M., Goff, J.C., Horbury, A.D. & Sadooni, F.N., 2010. The Petroleum Geology of Iraq, Scientific Press Ltd, Beaconsfield, U.K. Authemayou, C., Bellier, O., Chardon, D., Benedetti, L., Malekzade, Z., Claude, C., Angeletti, B., Shabanian, E. & Abbassi, M. R., 2009. Quaternary slip-rates of the Kazerun and the Main Recent Faults: Active strike-slip partitioning in the Zagros fold-and-thrust belt, Geophys. J. Int., 178, 524-540, doi:10.1111/j.1365-246X.2009.04191.x. Authemayou, C., Chardon, D., Bellier, O., Malekzadeh, Z., Shabanian, F. & Abbassi, M.R., 2006. Late Cenozoic partitioning of oblique plate convergence in the Zagros fold-and-thrust belt (Iran), Tectonics, 25, TC3002, doi:10.1029/2005tc001860. Bahroudi, A. & Koyi, H. A., 2003. Effect of spatial distribution of Hormuz salt on deformation style in the Zagros fold and thrust belt: an analogue modelling approach, J. Geol. Soc. Lond., 160, 719–733. Barnhart, W.D. & Lohman, R.B., 2013. Vertical partitioning of strain during earthquake sequences in Iran: Phantom earthquakes and triggered aseismic creep, Geophys. Res. Lett., 40, 819-823, doi:10.1002/grl.50201. Barnhart, W.D., Lohman, R.B. & Mellors, R.J., 2013. Active accommodation of plate convergence in Southern Iran: Earthquake locations, triggered aseismic slip, and regional strain rates, J. Geophys. Res. Solid Earth, 118, 5699-5711, doi:10.1002/jgrb.50380. Berberian, M., 1995. Master blind thrust faults hidden under the Zagros folds: active basement tectonics and surface morphotectonics, Tectonophysics, 241, 193-224, doi:10.1016/0040-1951(94)00185-C. Beutler, G., Moore, A.W. & Mueller, I.I., 2008. The International Global Navigation Satellite Systems (GNSS) Service: developments and achievements, J. Geodesy, 83 (3-4), 297-307, doi:10.1007/s00190-008-0268-z. Bird, P., 2003. An updated digital model of plate boundaries, Geochemistry Geophysics Geosystems, 4(3), 1027, doi:10.1029/2001GC000252. Bosold, A., Schwarzhans, W., Julapour, A., Ashrazadeh, A.R. & Ehsani, S.M., 2005. The structural geology of the High Central Zagros revisisted (Iran), Pet. Geosci., 11, 225-238, doi:10.1144/1354-079304-646. Clarke, P.J., Davies, R.R., England, P.C., Parsons, B., Billiris, H., Paradissis, D., Veis, G., Cross, P. A., Denys, P. H., Ashkenazi, V., Bingley, R., Kahle, H.-G., Muller, M.-V. & Briole, P., 1998. Crustal strain in central Greece from repeated GPS measurements in the interval 1989-1997, Geophys. J. Int., 135, 195-214, doi:10.1046/j.1365-246X.1998.00633.x. Colman-Sadd, S., 1978. Fold development in Zagros simply folded belt, Southwest Iran. AAPG Bull.,62, 984-1003. Copley, A. & Jackson, J., 2006. Active tectonics of the Turkish-Iranian Plateau, Tectonics, 25, TC6006, doi:10.1029/2005TC001906. Davies, R., England, P., Parsons, B., Billiris, H., Paradissis, D. & Veis, G., 1997. Geodetic strain in Greece in the interval 1892-1992, J. Geophys. Res., 102, 24,571-24,588, doi:10.1029/97JB01644. Djamour, Y., Vernant, P., Nankali, H.R. & Tavakoli, F., 2011. NW Iran-eastern Turkey present-day kinematics: Results from the Iranian permanent GPS network, Earth Planet. Sci. Lett., 307 (1-2), 27-34, doi:10.1016/j.epsl.2011.04.029 Dziewonski, A.M., Chou, T.-A., & Woodhouse, J.H., 1981. Determination of earthquake source parameters from waveform data for studies of global and regional seismicity, J. Geophys. Res., 86, 2825-2852, doi:10.1029/JB086iB04p02825. Edgell, H.S, 1991. Proterozoic salt basins of the Persian Gulf area and their role in hydrocarbon generation, Precambrian Res., 54, 1-14, doi:10.1016/0301-9268(91)90065-I. Ekström, G., Nettles, M., & Dziewonski, A.M., 2012. The global CMT project 2004-2010: Centroid-moment tensors for 13,017 earthquakes, Phys. Earth Planet. Inter., 200-201, 1-9, doi:10.1016/j.pepi.2012.04.002. Elliott, J.R., Bergman, E.A., Copley, A.C., Ghods, A. R., Nissen, E. K., Oveisi, B., Tatar, M., Walters, R. J., & Yamini-Fard, F., 2015. The 2013 Mw 6.2 Khaki-Shonbe (Iran) Earthquake: Insights into seismic and aseismic shortening of the Zagros sedimentary cover, Earth and Space Sci., 2, 435-471, doi:10.1002/2015EA000098. Engdahl, R. E., Jackson, J. A., Myers, S. C., Bergman, E. A. & Priestley, K. 2006. Relocation and assessment of seismicity in the Iran region, Geophys. J. Int., 167, 761-778. doi:10.1111/j.1365-246X.2006.03127.x Frohlich, C., 1992. Triangle diagrams: ternary graphs to display similarity and diversity of earthquake focal mechanisms, Phys. Earth Planet. Inter., 75, 193-198, doi:10.1016/0031-9201(92)90130-N. Ghasemi, A. & Talbot, C. J. 2006. A new tectonic scenario for the Sanandaj-Sirjan Zone (Iran), J. Asian Earth Sci., 26, 683-693, doi:10.1016/j.jseaes.2005.01.003. Goldsmith, N.F., Martinell, J., Demarcq, G., Bohn-Havas, M. & Dockery D.T. III, 1994. Sr-isotopic calibration of Cenozoic bivalvia and Early Miocene migrations: Eurasian Carnivores to Africa (the Hazeva Formation, Israel) and African gazelles and proboscidia to Ipolytarnoc, Hungary. Newslett. Stratigraphy, 31 (3), 167-183. Guest, B., Stockli, D.F., Grove, M., Axen, G.J., Lam, P.S. & Hassanzadeh, J., 2006. Thermal histories from the central Alborz Mountains, northern Iran: Implications for the spatial and temporal distribution of deformation in northern Iran, Geol. Soc. Am. Bull., 118, 1507-1521, doi:10.1130/B25819.1. Haines, A. J. & Holt W. E., 1993. A procedure for obtaining the complete horizontal motions within zones of distributed deformation from the inversion of strain rate data, J. Geophys. Res., 98, 12,057-12,082, doi:10.1029/93JB00892. Hanks, T.C., & Kanamori, H., 1979. A moment magnitude scale, J. Geophys. Res., 84, B5, 2348-2350, doi:10.1029/JB084iB05p02348. Hatzfeld, D. & Molnar, P., 2010. Comparisons of the kinematics and deep structures of the Zagros and Himalaya and of the Iranian and Tibetan plateaus and geodynamic implications, Rev. Geophys., 48, RG2005, doi:10.1029/2009RG000304. Hessami, K., Nilforoushan, F., & Talbot, C.J., 2006. Active deformation within the Zagros Mountains deduced from GPS measurements, J. Geol. Soc. London, 163 (1), 143-148. Hyndman, R. D., &Weichert, D. H., 1983. Seismicity and rates of relative plate motion on the plate boundaries of western North America, Geophys. J. R. Astron. Soc., 72, 59–82. Jackson, J., 1992. Partitioning of strike-slip and convergent motion between Eurasia and Arabia in eastern Turkey and the Caucasus, J. Geophys. Res., 97, 12471-12479. Jackson, J.A. & McKenzie, D.P., 1988. The relationship between plate motions and seismic tensors, and the rates of active deformation in the Mediterranean and Middle East, Geophys. J. R. astr. Soc., 93, 45-73. Jahani, S., Callot, J.P., Letouzey, J., & Frizon De Lamotte, D., 2009. The eastern termination of the Zagros fold-and-thrust belt, Iran: structures, evolution, and relationships between salt plugs, folding, and faulting, Tectonics, 28 (6), doi:10.1029/2008TC002418. Karimiparidari, S., Zaré, M., Memarian, H., & Kijko, A., 2013. Iranian earthquakes, a uniform catalog with moment magnitudes, J. Seismol., 17, 897-911, doi:10.1007/s10950-013-9360-9. Kennett, B.L.N., Engdahl, E.R. & Buland, R., 1995. Constraints on seismic velocities in the Earth from traveltimes. Geophys. J. Int., 122, 108-124, doi:10.1111/j.1365-246X.1995.tb03540.x. Kent, P.E., 1979. The emergent Hormuz salt plugs of southern Iran, J. Pet. Geol., 2, 117-144. Khodaverdian, A., Zafarani, H. & Rahimian, M., 2015. Long term fault slip rates, distributed deformation rates and forecast of seismicity in the Iranian Plateau, Tectonics, 34(10), 2190-2220. Kijko, A. & Singh, M., 2011. Statistical tools for maximum possible earthquake magnitude estimation. Acta Geophys., 59, 674-700, doi:10.2478/s11600-011-0012-6. Kostrov, B., 1974. Seismic moment and energy of earthquakes and seismic flow of rock, Izv. Acad. Sci. USSR, Phys. Solid Earth, 1, 23-40. Masson, F., Anvari, M., Djamour, Y., Walpersdorf, A., Tavakoli, F., Daignieres, M., Nankali, H. & Van Gorp, S., 2007. Large-scale velocity field and strain tensor in Iran inferred from GPS measurements: new insight for the present-day deformation pattern within NE Iran, Geophys. J. Int., 170, 436-440, doi:10.1111/j.1365-246X.2007.03477.x. Masson, F., Chéry, J., Hatzfeld, D., Martinod, J., Vernant, P., Tavakoli, F. & Ghafory-Ashtiani, M., 2005. Seismic versus aseismic deformation in Iran inferred from earthquakes and geodetic data, Geophys. J. Int., 160, 217-226, doi:10.1111/j.1365-246X.2004.02465.x. Mazhari, S.A., Bea, F., Amini, S., Ghalamghash, J., Molina, J.F., Montero, P., Scarrow, J.H. & Williams, I.S., 2009. The Eocene bimodal Piranshahr massif of the Sanandaj-Sirjan Zone, NW Iran: A marker of the end of the collision in the Zagros orogeny, J. Geol. Soc. London, 166, 53-69, doi:10.1144/0016-76492008-022. Mazzotti, S. & Adams, J., 2005. Rates and uncertainties on seismic moment and deformation in eastern Canada, J. Geophys. Res., 110, B09301, doi:10.1029/2004JB003510. Mazzotti, S., Leonard, L.J., Cassidy, J.F., Rogers, G.C. & Halchuk, S., 2011. Seismic hazard in western Canada from GPS strain rates versus earthquake catalog, J. Geophys. Res., 116, B12310, doi:10.1029/2011JB008213. McQuarrie, N. 2004. Crustal scale geometry of the Zagros fold-thrust belt, Iran, J. Struct. Geol., 26, 519-535. Melville, C., 1984. The use of Historical records for seismic assessment, Boll. Geofis. Teor. Appl., 26, 109-119. Mirzaei, N., Gao, M., Chen, Y.T. & Wang, J., 1997. A uniform catalog of earthquakes for seismic hazard assessment in Iran, ActaSeismol. Sinica, 10, 713-726. Molinaro, M., Zeyen, H. & Laurencin, X., 2004. Lithospheric structure beneath the southeastern Zagros Mountains, Iran: recent slab break‐off? Terra Nova, 17 (1), 1-6, doi:10.1111/j.1365-3121.2004.00575.x. Mousavi Z., Walpersdorf, A., Walker, R.T., Tavakoli, F., Pathier, E., Nankali, H., Nilfouroushan, F. & Djamour, Y., 2013. Global Positioning System constraints on the active tectonics of NE Iran and the South Caspian region, Earth Planet. Sci. Lett., 377-378, 287-298, doi:10.1016/j.epsl.2013.07.007. Mouthereau, F., Lacombe, O. &Vergés, J., 2012. Building the Zagros collisional orogeny: Timing, strain distribution and the dynamics of Arabia/Eurasia convergence, Tectonophysics, 532, 27-60, doi:10.1016/j.tecto2012.01.022. Mouthereau, F., Tensi, J., Bellahsen, N., Lacombe, O., De Boisgrollier, T. & Kargar, S., 2007. Tertiary sequence of deformation in a thin-skinned/thick-skinned collision belt: The Zagros folded belt (Fars, Iran), Tectonics, 26, Tc5006, doi:10.1029/2007tc002098. Nissen, E., Jackson, J., Jahani, S. & Tatar, M., 2014. Zagros “phantom earthquakes” reassessed - The interplay of seismicity and deep salt flow in the Simply Folded Belt? J. Geophys. Res. Solid Earth, 119, doi:10.1002/2013JB010796. Nissen, E., Tatar, M., Jackson, J.A. & Allen, M.B., 2011. New views on earthquake faulting in the Zagros fold-and-thrust belt of Iran, Geophys. J. Int., 186, 928-944, doi:10.1111/j.1365-246X.2011.05119.x. Okay, A.I., Zattin, M. & Cavazza, W., 2010. Apatite fission-track data for the Miocene Arabia-Eurasia collision, Geology, 38, 35-38, doi:10.1130/G30234.1. Palano, M., 2015. On the present-day crustal stress, strain-rate fields and mantle anisotropy pattern of Italy, Geophys. J. Int., 200 (2), 969-985, doi:10.1093/gji/ggu451. Palano, M., Imprescia, P. & Gresta, S., 2013. Current stress and strain-rate fields across the Dead Sea Fault System: Constraints from seismological data and GPS observations, Earth Planet. Sci. Lett., 369-370, 305-316, doi:10.1016/j.epsl.2013.03.043. Paul, A., Kaviani, A., Hatzfeld, D., Vergne, J. & Mokhtari, M., 2006. Seismological evidence for crustal-scale thrusting in the Zagros mountain belt (Iran), Geophys. J. Int., 166, 227-237, doi:10.1111/j.1365-246X.2006.02920.x. Peyret, M., Djamour, Y., Hessami, K., Regard, V., Bellier, O., Vernant, P., Daignicres, M., Nankali, H., Van Gorp, S., Goudarzi, M., Chéry, J., Bayer, R. & Rigoulay, M., 2009. Present-day strain distribution across the Minab-Zendan-Palami fault system from dense GPS transects, Geophys. J. Int., 179, 751-762, doi:10.1111/j.1365-246X.2009.04321.x. Reilinger, R., McClusky, S., Vernant, P., Lawrence, S., Ergintav, S., Cakmak, R., Ozener, H., Kadirov, F., Guliev, I., Stepanyan, R., Nadariya, M., Hahubia, G., Mahmoud, S., Sakr, K., ArRajehi, A., Paradissis, D., Al-Aydrus, A., Prilepin, M., Guseva, T., Evren, E., Dmitrotsa, A., Filikov, S.V., Gomez, F., Al-Ghazzi, R. & Karam, G., 2006. GPS constraints on continental deformation in the Africa-Arabia-Eurasia continental collision zone and implications for the dynamics of plate interactions, J. Geophys. Res., 111, B05411, doi:10.1029/2005JB004051. Sattarzadeh, Y., Cosgrove, J.W., & Vita-Finzi, C., 1999. The interplay of faulting and folding during the evolution of the Zagros deformation belt. In: Cosgrove, J.W., Ameen, M.S. (Eds.), Forced Folds and Fractures, Geol. Soc. Spec. Publ. London, 169, 187-196, doi:10.1144/GSL.SP.2000.169.01.14. Savage, J.C. & Simpson, R.W., 1997. Surface strain accumulation and the seismic moment tensor, Bull. Seismol. Soc. Am., 87, 1345-1353. Shen, Z.-K., Wang, M., Zeng, Y., Wang, F., 2015. Optimal interpolation of spatially discretized geodetic data, Bull. Seismol. Soc. Am., 105, 2117-2127, doi:10.1785/0120140247. Sherkati, S., Letouzey, J. & Frizon de Lamotte, D. 2006. Central Zagros fold-thrust belt (Iran): New insights from seismic data, field observation, and sandbox modeling, Tectonics, 25, TC4007, doi:10.1029/2004TC001766. Smith, W.H.F. & Wessel, P., 1990. Gridding with continuous curvature splines in tension, Geophysics, 55, 293-305. Talbot, C. J. & Alavi, M., 1996. The past of a future syntaxis across the Zagros. In: Alsop, G. I., Blundell, D. J., Davison, I. (Eds.), Salt Tectonics: Geol. Soc. Spec. Pub., 100, 89-109, doi:10.1144/GSL.SP.1996.100.01.08. Talebian, M. & Jackson, J., 2004. A reappraisal of earthquake focal mechanisms and active shortening in the Zagros mountains of Iran, Geophys. J. Int., 156, 506-526, doi:10.1111/j.1365-246X.2004.02092.x. Tavakoli, F., Walpersdorf, A., Authemayou, C., Nankali, H.R., Hatzfeld, D., Tatar, M., Djamour, Y., Nilforoushan, F. & Cotte, N., 2008. Distribution of the right‐lateral strike‐slip motion from the Main Recent Fault to the Kazerun fault system (Zagros, Iran): evidence from present‐day GPS velocities, Earth Planet. Sci. Lett., 275 (3-4), 342-347, doi:10.1016/j.epsl.2008.08.030. Tchernov, E., Ginsburg, L., Tassy, P. & Goldsmith, N.F., 1987. Miocene mammals of the Negev (Israel), J. Vertebr. Paleontol., 7 (3), 284-310. Walpersdorf, A., Hatzfeld, D., Nankali, H.R., Tavakoli, F., Nilforoushan, F., Tatar, M., Vernant, P., Chery, J. & Masson, F., 2006. Difference in the GPS deformation pattern of North and Central Zagros (Iran), Geophys. J. Int., 167, 1077-1088, doi:10.1111/j.1365-246X.2006.03147.x. Walpersdorf, A., Manighetti, I., Mousavi, Z., Tavakoli, F., Vergnolle, M., Jadidi, A., Hatzfeld, D., Aghamohammadi, A., Bigot, A., Djamour, Y., Nankali, H. & Sedighi, M., 2014. Present-day kinematics and fault slip rates in Eastern Iran, derived from 11 years of GPS data, J. Geophys. Res. Solid Earth, 119, 1359-1383, doi:10.1002/2013JB010620. Kijko, A. & Graham, G. 1998. Parametric-historic Procedure for Probabilistic Seismic Hazard Analysis Part I: Estimation of Maximum Regional Magnitude mmax, Pure appl. geophys., 154, 413-442, doi:10.1007/s000240050218. Wells, D. L. & Coppersmith, K. J., 1994. New empirical relationship among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bull. Seismol. Soc. Am., 84, 974-1002. Weichert, D. H., 1980. Estimation of the earthquake recurrence parameters from unequal observation periods for different magnitudes, Bull. Seismol. Soc. Am., 70, 1337-1346. Wessel, P. & Bercovici, D., 1998. Interpolation with splines in tension: a Green’s function approach, Math. Geol., 30, 77-93. Zarifi, Z., Nilfouroushan, F. & Raeesi, M., 2013. Crustal Stress Map of Iran: insight from seismic and geodetic computations, Pure Appl. Geophys., 171, 7, 1219-1236, doi:10.1007/s00024-013-0711-9. Zoback, M.L., 1992. First- and second-order patterns of stress in the lithosphere: The World Stress Map Project, J. Geophys. Res., 97 (B8), 11703-11728, doi:10.1029/92JB00132. | en |
| dc.description.obiettivoSpecifico | 2T. Deformazione crostale attiva | en |
| dc.description.journalType | JCR Journal | en |
| dc.relation.issn | ISSN 0956-540X | en |
| dc.relation.eissn | 1365-246X | en |
| dc.contributor.author | Palano, Mimmo | en |
| dc.contributor.author | Imprescia, Paola | en |
| dc.contributor.author | Agnon, Amotz | en |
| dc.contributor.author | Gresta, Stefano | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | en |
| dc.contributor.department | Istituto di Geologia Ambientale e Geoingegneria, Consiglio Nazionale delle Ricerche, Roma, Italia | en |
| dc.contributor.department | Fredy & Nadine Herrmann Institute of Earth Sciences, The Hebrew University, 91904 Jerusalem, Israel | en |
| dc.contributor.department | Dipartimento di Scienze Biologiche, Geologiche e Ambientali, Universit`a degli Studi di Catania, Catania, Italia | en |
| item.openairetype | article | - |
| item.cerifentitytype | Publications | - |
| item.languageiso639-1 | en | - |
| item.grantfulltext | open | - |
| item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
| item.fulltext | With Fulltext | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia | - |
| crisitem.author.dept | Istituto di Geologia Ambientale e Geoingegneria, Consiglio Nazionale delle Ricerche, Roma, Italia | - |
| crisitem.author.dept | Fredy & Nadine Herrmann Institute of Earth Sciences, The Hebrew University, 91904 Jerusalem, Israel | - |
| crisitem.author.dept | Università di Catania | - |
| crisitem.author.orcid | 0000-0001-7254-7855 | - |
| crisitem.author.orcid | 0000-0002-0232-8574 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
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| 2018_Palano et al [Zagros Seismic Coupling] GJI.pdf | pubblished paper | 4.22 MB | Adobe PDF | View/Open |
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