...-volcanic gas to the surface. In this study, we have analyzed the correlation between the active tectonic framework of the Matese Ridge area and the high gas emissions found to the southwest, which includes large amounts of CO 2 (up to 99 vol%), CH 4 (up to 0.55 vol%), and He (up to 52 ppmv). We measured CO...

... G. Pierattini D. Tarling D.H. Morris A. Tarling D.H. Paleomagnetic evidence of block rotation in the Matese Mountains, Southern Apennine, Italy Paleomagnetism and Tectonics of the Mediterranean Region 1996 105 London Geological Society 133 139 Special Publications...

... , A. , 2019 , Constraining mountain front tectonic activity in extensional setting from geomorphology and Quaternary stratigraphy: A case study from the Matese ridge, southern Apennines : Quaternary Science Reviews , v. 219 , p. 47 – 67 , https://doi.org/10.1016/j.quascirev.2019.07.001 . Vitale...

...Fig. 3. Early Pleistocene configuration. CL, Campania–Lucania arc; ECA, External Calabrian Arc; MAR, Mid-Adriatic ridge; MB, Matese–Benevento arc; ST, Southern Tyrrhenian basin. Symbols, colours and other abbreviations as in Figure 2 . ...

... Working Group, 2006 ). Although ridge-top normal faulting accounts for much of the seismicity of peninsular Italy, several major earthquakes that took place in central and southern Italy contrast with this simple model (e.g., 1361, 1466, 1627, 1694, 1731, 1930, 1981; see Table 1 for corresponding ID...

... and includes several carbonate units separated by thrust surfaces; iii) Lagonegro-Molise Basin; this wide basin was located between the Apenninic Platform and the Apulia Platform and includes several pelagic successions and turbidite units (e.g., Agnone Flysch); iv) Simbruini-Matese Platform; it includes...

... et al . 1998 ; Chiodini et al . 1999 ; Caliro et al . 2005 ). Hence, studying the concentration of total dissolved inorganic carbon (TDIC) in groundwater is a suitable way to infer the regional flux of endogenous CO 2 . The Apennines are a series of mountain ridges that run the entire length...

... to their paleogeographic positions. The first orogenic event recorded in the continental part of the Adria plate was the Oligocene forebulge stage that produced uplift and erosion of the Apennine Platform and sedimentation in the surrounding basins. Subsequently, the forebulge ridge migrated toward E/NE ( Sabbatino et al...

... and those forced by solar torques. We suggest that the 273 m.yr. period reflects the cosmic year. The latter modulates fluctuation in cometary impacts that occur with a 30–35 m.yr. period (Matese et al. 1996 ). Thus, there may be more than one driving force for mantle plume volcanism, including forces...

... ( 2007 ), C osentino et alii ( 2010 ) and V ezzani et alii ( 2010 ); from West to East they are (starting age of activity in brackets): Sibillini (late Tortonian); Lepini-Ausoni-Aurunci (late Tortonian); Simbruini-Ernici-Matese (early Messinian); Gran Sasso-Western Marsica (late Messinian); Morrone...

... depression, surrounded to the north and west by the carbonate massifs of Matese, Taburno and Avella, and to the east and south by the low ridges of the Sannita Apennine. The Calore river and its tributaries (Miscano, Ufita, Tammaro and Sabato rivers) flow between these two ridges, along long valleys, to end...

.... Subgeneric diagnosis rephrased from Kollmann ( 1967 ) and Sohl and Kollmann ( 1985 ): the greatest shell width is above mid-height, and the spire comprises less than half of the total shell height. The aperture is narrow, parietal lip smooth; columella with three plaits, one as a high palatal ridge...

... . From R , we obtained the local relief using the Focal Statistics tool with the range statistic over a 2.5 km rectangular neighborhood. We choose this window assuming that it captures the most common ridge-valley spacing (along the coast). The resulting map is shown in Figure 4 (a). According...

... & Hillgärtner 1998) provides a dynamic picture of their depositional history and may allow a clearer understanding of the relationship between relative sea-level oscillations and sedimentation. Pleistocene uplift produced mountains more than 1000 m above sea-level, like the ridges of Monte S. Angelo a Tre...

...; the LV myophores are expanded plates on the valve wall; on the RV the posterior myophore plate extends from the cardinal platform; RV posterior tooth a large arcuate ridge. The subfamily includes Matheronia (and its subgenus Monnieria ), Hypelasma , Lovetchenia , Rutonia , and Kugleria . Genus...

... 41 NOR NORCIA 42.7924 13.0924 B * 3 42 ORC ORTUCCHIO 41.9540 13.6420 A * 11 43 PDM PIEDIMONTE MATESE 41.3550 14.3850 C * 1 44 PIC PIANCASTAGNAIO 42.8500 11.6850 B * 2 45 PSC PESCASSEROLI 41.8120 13.7892 A * 2 46 PTF PETRELLA TIFERNINA...

... of the anterior tooth, C=canals, CT=central tooth, ct=socket of the central tooth, DC=dorsal cavity, iOSL=inner part of the outer shell layer, IMG=inner marginal groove, ISL=inner shell layer, L=ligamental ridge, LV=left valve, MC=main body cavity, OSL=outer shell layer, oOSL=outer part of outer shell layer, P1...

... ; Galli and Peronace, 2014 ; Gori et al., 2011 ; Mirabella et al., 2011 ; Roberts and Michetti, 2004 ; Schirripa Spagnolo et al., 2021 ; Sgambato et al., 2020 ; Villani et al., 2018 ; Villani and Pierdominici, 2010 ). In some cases, these structures run in the highest portions of the main ridges...