Abstract
The historical seismicity catalogs report that the Gargano area (Apulia region, southern Italy) has been site of medium to high magnitude earthquakes. Instrumental seismicity suffers of the poor coverage of the seismic stations of the RSN (National Seismic Network). To improve the seismological monitoring of the area, in 2013 the OTRIONS seismic network (OSN), managed by the University of Bari - Italy, in cooperation with INGV (National Institute of Geophysics and Volcanology), was installed. In this study, focal mechanisms of single and composite events have been computed using 118 micro-earthquakes occurred in this area. We subdivided the dataset into subsets according to their location and depth, distinguishing between the Promontory zone and the Apulian foredeep. High quality focal mechanisms and low-misfit stress tensor inversion were obtained for three groups of events. To better constrain the stress tensor we included also focal mechanism solutions obtained in previous studies. In the southwestern Apulian foredeep zone, a normal fault kinematics is inferred, normal to the Apennine stress direction; in the Promontory zone, the fault kinematics indicate inverse fault mechanisms striking in NE-SW direction. Differently from previous analyses, the stress orientations inferred in this study agree with those inferred in the World Stress Map.
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References
Bath, M., Duda, S.J.: Earthquake volume, fault plane area, seismic energy, strain, deformation and related quantities. Ann. Geofis. 17(3), 353–368 (1964). https://doi.org/10.4401/ag-5213
Bertotti, G., Casolari, E., Picotti, V.: The Gargano Promontory, a contractional belt. Terra Nova 11, 168–173 (1999). https://doi.org/10.1046/j.1365-3121.1999.00243.x
Billi, A., Gambini, R., Nicolai, C., Storti, F.: Neogene-Quaternary intraforeland transpression along a Mesozoic platform-basin margin: the Gargano fault system, Adria, Italy. Geosphere 3(1), 1–15 (2007). https://doi.org/10.1130/GES00057.1
Borre, K., et al.: The COST project in Italy: analysis and monitoring of seismogenic faults in the Gargano and Norcia areas (central-southern Apennines, Italy). J. Geodyn. 36(1–2), 3–18 (2003). https://doi.org/10.1016/S0264-3707(03)00035-8
Brankman, C.M., Aydin, A.: Uplift and contractional deformation along a segmented strike-slip fault system: the Gargano Promontory, southern Italy. J. Struct. Geol. 26, 807–824 (2004). https://doi.org/10.1016/j.jsg.2003.08.018
Calcagnile, G., Panza, G.F.: The main characteristics of the lithosphere-asthenosphere system in Italy and surroundings regions. Pure. appl. Geophys. 119(4), 865–879 (1980). https://doi.org/10.1007/BF01131263
Chilovi, C., De Feyter, A.J., Pompucci, A.: Wrench zone reactivation in the Adriatic block: the example of the Mattinata fault system (SE Italy). Boll. Soc. Geol. It. 119, 3–8 (2000)
de Lorenzo, S., Michele, M., Emolo, A., Tallarico, A.: A 1D P-wave velocity model of the Gargano promontory (southeastern Italy). J. Seismol. 21(4), 909–919 (2017). https://doi.org/10.1007/s10950-017-9643-7
Del Gaudio, V., Pierri, P., Frepoli, A., Calcagnile, G., Venisti, N., Cimini, G.: A critical revision of the seismicity of northern Apulia (Adriatic microplate - Southern Italy) and implications for the identification of seismogenic structures. Tectonophysics 436(1–4), 9–35 (2007). https://doi.org/10.1016/j.tecto.2007.02.013
Di Bucci, D., Mazzoli, S.: The October-November 2002 Molise seismic sequence (southern Italy): an expression of Adria intraplate deformation. J. Geol. Soc. Lond. 160(4), 503–506 (2003)
Doglioni, C., Mongelli, F., Pieri, P.: The Puglia uplift (SE Italy): an anomaly in the foreland or the Apenninic subduction due to buckling or a thick continental lithosphere. Tectonics 13(5), 1309–1321 (1994). https://doi.org/10.1029/94TC01501
Favali, P., Funiciello, R., Mattietti, G., Mele, G., Salvini, F.: An active margin across the Adriatic Sea (central Mediterranean Sea). Tectonophysics 219, 109–117 (1993). https://doi.org/10.1016/0040-1951(93)90290-Z
Filippucci, M., Tallarico, A., Dragoni, M., de Lorenzo, S.: Relationship between depth of seismicity and heat flow: the case of the Gargano area (Italy). Pure. appl. Geophys. 176(6), 2383–2394 (2019a). https://doi.org/10.1007/s00024-019-02107-5
Filippucci, M., Del Pezzo, E., de Lorenzo, S., Tallarico, A.: 2D kernel-based imaging of coda-Q space variations in the Gargano Promontory (Southern Italy). Phys. Earth Planet. Int. 297, 106313 (2019b). https://doi.org/10.1016/j.pepi.2019.106313
Frepoli, A., Amato, A.: Spatial variation in stresses in peninsular Italy and Sicily from background seismicity. Tectonophysics 317(1–2), 109–124 (2000). https://doi.org/10.1016/S0040-1951(99)00265-6
Gephart, J.W.: FMSI: a FORTRAN program for inverting fault/slickenside and earthquake focal mechanism data to obtain the regional stress tensor. Comput. Geosci. 16, 953–989 (1990). https://doi.org/10.1016/0098-3004(90)90105-3
Heidbach, O., et al.: The World Stress Map database release 2016: crustal stress pattern across scales. Tectonophysics 744, 484–498 (2018). https://doi.org/10.1016/j.tecto.2018.07.007
Imanishi, K., et al.: Depth-dependent stress field in and around the Atotsugawa fault, central Japan, deduced from microearthquake focal mechanisms: evidence for localized aseismic deformation in the downward extension of the fault. J. Geophys. Res. 116, B01305 (2011). https://doi.org/10.1029/2010JB007900
Lu, Z., Wyss, M., Pulpan, H.: Details of stress directions in the Alaska subduction zone from fault plane solutions. J. Geophys. Res. 102(B3), 5385–5402 (1997). https://doi.org/10.1029/96JB03666
Milano, G., Di Giovambattista, R., Ventura, G.: Seismic constraints on the present-day kinematics of the Gargano foreland, Italy, at the transition zone between the southern and northern Apennine belts. Geophys. Res. Lett. 32, L24308 (2005). https://doi.org/10.1029/2005GL024604
Montone, P., Mariucci, M.T.: The new release of the Italian contemporary stress map. Geophys. J. Int. 205(3), 1525–1531 (2016). https://doi.org/10.1093/gji/ggw100
Patacca, E., Scandone, P.: Identificazione e valutazione di strutture sismogenetiche. Rapporto tecnico, Convenzione ENEA - Dipartimento di Scienze della Terra Università di Pisa, Italy (2001)
Patacca, E., Scandone, P.: The 1627 Gargano earthquake (Southern Italy): identification and characterization of the causative fault. J. Seismol. 8(2), 259–273 (2004). https://doi.org/10.1023/B:JOSE.0000021393.77543.1E
Reasenberg, P., Oppenheimer, D.: FPFIT, FPPLOT and FPPAGE: FORTRAN computer programs for calculating and displaying earthquake fault-plane solutions. USGS Open-File Rep., 85–739 (1985). https://doi.org/10.3133/ofr85739
Roselli, P., Marzocchi, W., Mariucci, M.T., Montone, P.: Earthquake focal mechanism forecasting in Italy for PSHA purposes. Geophys. J. Int. 212(1), 491–508 (2018). https://doi.org/10.1093/gji/ggx383
Rovida, A., Locati, M., Camassi, R., Lolli, B., Gasperini, P.: Catalogo Parametrico dei Terremoti Italiani (CPTI15), versione 2.0. Istituto Nazionale di Geofisica e Vulcanologia (INGV) (2019). https://doi.org/10.13127/CPTI/CPTI15.2
Salvi, S., et al.: A multidisciplinary approach to earthquake research: implementation of a geochemical geographic information system for the Gargano site, Southern Italy. Nat. Haz. 20, 255–278 (1999). https://doi.org/10.1023/A:1008105621134
Tondi, E., Piccardi, L., Cacon, S., Kontny, B., Cello, G.: Structural and time constraints for dextral shear along the seismogenic Mattinata Fault (Gargano, southern Italy). J. Geodyn. 40(2–3), 134–152 (2005). https://doi.org/10.1016/j.jog.2005.07.003
Tripaldi, S.: Electrical signatures of a permeable zone in carbonates hosting local geothermal manifestations: insights for the deep fluid flow in the Gargano area (south-eastern Italy). Boll. Geof. Teor. Appl. 61(2), 219–232 (2020). https://doi.org/10.4430/bgta0312
Valensise, G., Pantosti, D., Basili, R.: Seismology and tectonic setting of the 2002 Molise, Italy, Earthquake. Earthq. Spectra 20, 23–37 (2004). https://doi.org/10.1193/1.1756136
Wessel, P., Smith, W.H.F.: New, improved version of Generic Mapping Tools released. Eos, Trans. Am. Geophys. Un. 79(47), 579 (1998). https://doi.org/10.1029/98EO00426
Zoback, M.L.: First and second order patterns of stress in the lithosphere: the World Stress Map Project. J. Geophys. Res. 97, 11703–11728 (1992). https://doi.org/10.1029/92JB00132
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Figures were obtained by employing the GMT freeware package by Wessel and Smith (1998) and by the Google Earth Pro, Google, Inc. California.
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Appendix
Locations of events of G1, G2 and G3groups, plotted in Fig. 3. For each event the id. number (Id), the origin (Date and Time, N Lat, E Lon and Depth), the magnitude (Ml), the residual (RMS), the horizontal and vertical errors (ERZ, ERH), the number of recording stations (Nstat), the number of recognized polarities (Npol) are reported.
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Filippucci, M., Pierri, P., de Lorenzo, S., Tallarico, A. (2020). The Stress Field in the Northern Apulia (Southern Italy), as Deduced from Microearthquake Focal Mechanisms: New Insight from Local Seismic Monitoring. In: Gervasi, O., et al. Computational Science and Its Applications – ICCSA 2020. ICCSA 2020. Lecture Notes in Computer Science(), vol 12255. Springer, Cham. https://doi.org/10.1007/978-3-030-58820-5_66
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