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Behaviour of minor arcuate shapes hosted in curved fold-and-thrust belts: an example from the Northern Apennines (Italy)

Published online by Cambridge University Press:  28 January 2019

Sara Satolli Open the ORCID record for Sara Satolli [Opens in a new window] ,
Simone Agostini  and
Fernando Calamita Open the ORCID record for Fernando Calamita [Opens in a new window]
Sara Satolli*
Affiliation:
Dipartimento di Ingegneria e Geologia, Università “G. d’Annunzio” di Chieti-Pescara, 66100 Chieti Scalo, Italy CiMaN-LP – Alpine Laboratory of Paleomagnetism, Via Luigi Massa 4, 12016, Peveragno (CN), Italy
Simone Agostini
Affiliation:
CGG Robertson – Tyn-y-Coed, Pentywyn Road, Llandudno, Gwynedd, UK
Fernando Calamita
Affiliation:
Dipartimento di Ingegneria e Geologia, Università “G. d’Annunzio” di Chieti-Pescara, 66100 Chieti Scalo, Italy
*
Author for correspondence: Sara Satolli, Email: [email protected]
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Abstract

Arcuate fold-and-thrust belts have been extensively studied in the literature. Less attention, however, has been paid to the characteristics of local-scale arcuate structures, meaning 5–10 km long fold or thrust traces that display map-view curvature. Nevertheless, detailed investigation of small arcuate structures hosted in major arcs can contribute to understanding the pervasiveness of deformation mechanisms. We performed a combined geological and palaeomagnetic study on 21 sites from a c. 60 km2 area in the Northern Apennines in order to analyse minor arcs at a kilometric scale. As evidenced by the geological and structural analysis performed on the 21 sites, the fold axial trend changes from N–S to NW–SE in the study area. The comparison with palaeomagnetic results shows the lack of correlation between vertical axis rotations and fold axial trends. As a consequence, the minor arcuate shapes of thrusts and related folds are interpreted as mostly primary features inherited from the geometry of the palaeomargin, represented by pre-orogenic faults, according to a context of inversion tectonics.

Keywords

inversion tectonicspalaeomagnetismstructural geologyvertical axis rotations
Type
Original Article
Information
Geological Magazine , Volume 156 , Issue 9 , September 2019 , pp. 1547 - 1564
Copyright
© Cambridge University Press 2019 

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References

Aiello, IW, Hagstrum, JT and Principi, G (2004) Late Miocene remagnetization within the internal sector of the Northern Apennines, Italy. Tectonophysics 383, 1–14.CrossRefGoogle Scholar
Alvarez, W (1990) Pattern of extensional faulting in pelagic carbonates of the Umbria-Marche Apennines of central Italy. Geology 18, 407–10.2.3.CO;2>CrossRefGoogle Scholar
Aubourg, C, Smith, B, Bakhtari, H, Guya, N, Eshragi, A, Lallemant, S, Molinaro, M, Braud, X and Delaunay, S (2004) Post-Miocene shortening pictured by magnetic fabric across the Zagros-Makran syntaxis (Iran). In Orogenic Curvature: Integrating Paleomagnetic and Structural Analyses (eds Sussman, AJ & Weil, AB), pp. 17–40. Boulder, Colorado: Geological Society of America, Special Paper 383.CrossRefGoogle Scholar
Bally, AW, Burbi, L, Cooper, C and Ghelardoni, R (1986) Balanced sections and seismic reflection profiles across the central Apennines. Memorie della Società Geologica Italiana 107, 109–30.Google Scholar
Barchi, MR (2010) The Neogene-Quaternary evolution of the Northern Apennines: crustal structure, style of deformation and seismicity. Journal of the Virtual Explorer 36, paper 11. doi: 10.3809/jvirtex.2010.00220.CrossRefGoogle Scholar
Barchi, MR, Boscherini, A, Collettini, C, Deiana, G, De Paola, N, Mirabella, F, Motti, A and Pierantoni, PP (2012) A geological map of the Colfiorito area (Umbria-Marche Apennines, Italy). Scale 1:25,000. Convegno FIST GeoItalia 01, Volume dei Riassunti, 333–4.Google Scholar
Barchi, MR, Minelli, G and Pialli, G (1998) The CROP 03 profile: a synthesis of results on deep structures of the Northern Apennines. Memorie della Società Geologica Italiana 52, 383–400.Google Scholar
Bayona, G, Thomas, WA and Van der Voo, R (2003) Kinematics of thrust sheets within transverse zones: a structural and paleomagnetic investigation in the Appalachian thrust belt of Georgia and Alabama. Journal of Structural Geology 25, 1193–212.CrossRefGoogle Scholar
Besse, J and Courtillot, V (2002) Apparent and true polar wander and the geometry of the geomagnetic field over the last 200 Myr. Journal of Geophysical Research: Solid Earth 107, 2300. doi: 10.1029/2000JB000050.CrossRefGoogle Scholar
Billi, A and Tiberti, MM (2009) Possible causes of arc development in the Apennines, central Italy. Bulletin of the Geological Society of America 121, 1409–20.CrossRefGoogle Scholar
Boccaletti, M, Calamita, F and Viandante, MG (2005) The lithospheric Apennine Neo-Chain developing since the Lower Pliocene as a result of the Africa-Europe convergence. Bollettino della Societa Geologica Italiana 124, 87–105.Google Scholar
Boccaletti, M, Ciaranfi, N, Cosentino, D, Deiana, G, Gelati, R, Lentini, F, Massari, F, Moratti, G, Pescatore, T, Ricci Lucchi, F and Tortorici, L (1990) Palinspastic restoration and paleogeographic reconstruction of the peri-Tyrrhenian area during the Neogene. Palaeogeography, Palaeoclimatology, Palaeoecology 77, 41–50.CrossRefGoogle Scholar
Calamita, F (1990) Thrusts and fold-related structures in the Umbria-Marche Apennines (Central Italy). Annales Tectonicae 4, 83–117.Google Scholar
Calamita, F, Coltorti, M, Piccinini, D, Pierantoni, PP, Pizzi, A, Ripepe, M, Scisciani, V and Turco, E (2000) Quaternary faults and seismicity in the Umbro-Marchean Apennines (Central Italy): evidence from the 1997 Colfiorito earthquake. Journal of Geodynamics 29, 245–64.CrossRefGoogle Scholar
Calamita, F, Coltorti, M, Pierantoni, PP, Pizzi, A, Scisciani, V and Turco, E (1997) Relazioni tra le faglie Quaternarie e la sismicita’ nella dorsale Appenninica umbro-marchigiana; l’area di Colfiorito. Studi Geologici Camerti 14, 177–91.Google Scholar
Calamita, F and Deiana, G (1988) The arcuate shape of the Umbria-Marche-Sabina Apennines (central Italy). Tectonophysics 146, 139–47.CrossRefGoogle Scholar
Calamita, F, Pace, P and Satolli, S (2012) Coexistence of fault-propagation and fault-bend folding in curve-shaped foreland fold-and-thrust belts: examples from the Northern Apennines (Italy). Terra Nova 24, 396–406.CrossRefGoogle Scholar
Calamita, F and Pierantoni, PP (1993) Il sovrascorrimento di M. Cavallo - M. Primo (Appennino umbro - marchigiano). Bollettino della Societa Geologica Italiana 112, 825–35.Google Scholar
Calamita, F and Pizzi, A (1994) Recent and active extensional tectonics in the southern Umbro-Marchean Apennines (Central Italy). Memorie della Società Geologica Italiana 48, 541–8.Google Scholar
Calamita, F, Satolli, S, Scisciani, V, Esestime, P and Pace, P (2011) Contrasting styles of fault reactivation in curved orogenic belts: examples from the central Apennines (Italy). Bulletin of the Geological Society of America 123, 1097–111.CrossRefGoogle Scholar
Calamita, F, Viandante, MG and Hegarty, K (2004) Pliocene-Quaternary burial/exhumation paths of the Central Apennines (Italy); implications for the definition of the deep structure of the belt. Bollettino della Societa Geologica Italiana 123, 503–12.Google Scholar
Carey, SW (1955) The orocline concept in geotectonics – Part I. Papers and Proceedings of the Royal Society of Tasmania 89, 255–89.Google Scholar
Caricchi, C, Cifelli, F, Sagnotti, L, Sani, F, Speranza, F and Mattei, M (2014) Paleomagnetic evidence for a post-Eocene 90° CCW rotation of internal Apennine units: a linkage with Corsica-Sardinia rotation? Tectonics 33, 374–92.CrossRefGoogle Scholar
Carmignani, L and Kligfield, R (1990) Crustal extension in the northern Apennines: the transition from compression to extension in the Alpi Apuane core complex. Tectonics 9, 1275–303.CrossRefGoogle Scholar
Channell, JET (1992) Paleomagnetic data from Umbria (Italy): implications for the rotation of Adria and Mesozoic apparent polar wander paths. Tectonophysics 216, 365–78.CrossRefGoogle Scholar
Channell, JET, Lowrie, W, Medizza, F and Alvarez, W (1978) Palaeomagnetism and tectonics in Umbria, Italy. Earth and Planetary Science Letters 39, 199–210.CrossRefGoogle Scholar
Channell, JET and McCabe, C (1994) Comparison of magnetic hysteresis parameters of unremagnetized and remagnetized limestones. Journal of Geophysical Research 99, 4613–23.CrossRefGoogle Scholar
Channell, JET, Oldow, JS, Catalano, R and D’Argenio, B (1990) Paleomagnetically determined rotations in the western Sicilian fold and thrust belt. Tectonics 9, 641–60.CrossRefGoogle Scholar
Cifelli, F, Caricchi, C and Mattei, M (2016) Formation of arc-shaped orogenic belts in the Western and Central Mediterranean: a palaeomagnetic review. In Palaeomagnetism in Fold and Thrust Belts: New Perspectives (eds Pueyo, EL, Citelli, F, Sussman, AJ & Olivia-Urci, B), pp. 37–63. Geological Society of London, Special Publication no. 425.Google Scholar
Cifelli, F and Mattei, M (2010) Curved orogenic systems in the Italian Peninsula: a paleomagnetic review. Journal of the Virtual Explorer 36, paper 17. doi: 10.3809/jvirtex.2010.00239.CrossRefGoogle Scholar
Cipollari, P and Cosentino, D (1995) Miocene unconformities in the Central Apennines: geodynamic significance and sedimentary basin evolution. Tectonophysics 252, 375–89.CrossRefGoogle Scholar
Coccioni, R, Franchi, R, Nesci, O, Perilli, N, Wezel, FC and Battistini, F (1989) Stratigrafia, micropaleontologia e mineralogia delle Marne a Fucoidi (Aptiano inferiore-Albiano superiore) delle sezioni di Poggio le Guaine e del Fiume Bosso (Appennino Umbro-Marchigiano). In Atti II convegno Internazionale ‘Fossili, Evoluzione, Ambiente’, Pergola, pp. 163–201.Google Scholar
Cogné, JP (2003) PaleoMac: a Macintosh ™ application for treating paleomagnetic data and making plate reconstructions. Geochemistry, Geophysics, Geosystems 4, 1007. doi: 10.1029/2001GC000227.CrossRefGoogle Scholar
Coward, MP, De Donatis, M, Mazzoli, S, Paltrinieri, W and Wezel, FC (1999) Frontal part of the northern Apennines fold and thrust belt in the Romagna-Marche area (Italy): shallow and deep structural styles. Tectonics 18, 559–74.CrossRefGoogle Scholar
Davis, D, Suppe, J and Dahlen, FA (1983) Mechanics of fold-and-thrust belts and accretionary wedges. Journal of Geophysical Research 88, 1153–72.CrossRefGoogle Scholar
Deamer, GA and Kodama, KP (1990) Compaction-induced inclination shallowing in synthetic and natural clay-rich sediments. Journal of Geophysical Research 95, 4511–29.CrossRefGoogle Scholar
Demarest, HH (1983) Error analysis for the determination of tectonic rotation from paleomagnetic data. Journal of Geophysical Research 88, 4321–8.CrossRefGoogle Scholar
Di Domenica, A, Turtù, A, Satolli, S and Calamita, F (2012) Relationships between thrusts and normal faults in curved belts: new insight in the inversion tectonics of the Central-Northern Apennines (Italy). Journal of Structural Geology 42, 104–17.CrossRefGoogle Scholar
Doglioni, C (1991) A proposal for the kinematic modelling of W-dipping subductions – possible applications to the Tyrrhenian-Apennines system. Terra Nova 3, 423–34.CrossRefGoogle Scholar
Eldredge, S, Bachtadse, V and Van Der Voo, R (1985) Paleomagnetism and the orocline hypothesis. Tectonophysics 119, 153–79.CrossRefGoogle Scholar
Enkin, RJ and Watson, GS (1996) Statistical analysis of palaeomagnetic inclination data. Geophysical Journal International 126, 781–95.CrossRefGoogle Scholar
Faccenna, C, Davy, P, Brun, JP, Funiciello, R, Giardini, D, Mattei, M and Nalpas, T (1996) The dynamics of back-arc extension: an experimental approach to the opening of the Tyrrhenian Sea. Geophysical Journal International 126, 781–95.CrossRefGoogle Scholar
Faccenna, C, Piromallo, C, Crespo-Blanc, A, Jolivet, L and Rossetti, F (2004) Lateral slab deformation and the origin of the western Mediterranean arcs. Tectonics 23, TC1012. doi: 10.1029/2002TC001488.CrossRefGoogle Scholar
Finetti, IR (2005) CROP PROJECT: Deep Seismic Exploration of the Central Mediterranean and Italy. Amsterdam: Elsevier, 794 pp.Google Scholar
Fisher, R (1953) Dispersion on a sphere. Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences 217, 195–305.CrossRefGoogle Scholar
Fossen, H (2010) Structural Geology. Cambridge: Cambridge University Press, 463 pp.CrossRefGoogle Scholar
Gattacceca, J and Speranza, F (2002) Paleomagnetism of Jurassic to Miocene sediments from the Apenninic carbonate platform (southern Apennines, Italy): evidence for a 60° counterclockwise Miocene rotation. Earth and Planetary Science Letters 201, 19–34.CrossRefGoogle Scholar
Gradstein, FM, Ogg, JG, Schmitz, MD, Ogg, GM, Gradstein, FM and All, A (2012) The Geologic Time Scale 2012. Amsterdam: Elsevier, 1176 pp.Google Scholar
Hindle, D and Burkhard, M (1999) Strain, displacement and rotation associated with the formation of curvature in fold belts; the example of the Jura arc. Journal of Structural Geology 21, 1089–101.CrossRefGoogle Scholar
Jackson, KC (1990) A palaeomagnetic study of Apennine thrusts, Italy: Monte Maiella and Monte Raparo. Tectonophysics 178, 231–40.CrossRefGoogle Scholar
Johnston, ST and Mazzoli, S (2009) The Calabrian Orocline: buckling of a previously more linear orogen. In Ancient Orogens and Modern Analogues (eds Murphy, JB, Keppie, JD & Hynes, AJ), pp. 113–25. Geological Society of London, Special Publication no. 327.Google Scholar
Jolivet, L, Dubois, R, Fournier, M, Goffe, B, Michard, A and Jourdan, C (1990) Ductile extension in alpine Corsica. Geology 18, 1007–10.2.3.CO;2>CrossRefGoogle Scholar
Kirschvink, JL (1980) The least-squares line and plane and the analysis of palaeomagnetic data. Geophysical Journal of the Royal Astronomical Society 62, 699–718.CrossRefGoogle Scholar
Koymans, MR, Langereis, CG, Pastor-Galán, D and van Hinsbergen, DJJ (2016) Paleomagnetism.org: an online multi-platform open source environment for paleomagnetic data analysis. Computers and Geosciences 93, 127–37.CrossRefGoogle Scholar
Kwon, S and Mitra, G (2004) Strain distribution, strain history, and kinematic evolution associated with the formation of arcuate salients in fold-thrust belts; the example of the Provo salient, Sevier orogen, Utah. In Orogenic Curvature – Integrating Paleomagnetic and Structural Analyses (eds Sussman, AJ & Weil, AB), pp. 205–23. Boulder, Colorado: Geological Society of America, Special Paper 383.CrossRefGoogle Scholar
Lacombe, O, Mouthereau, F, Angelier, J, Chu, HT and Lee, JC (2003) Frontal belt curvature and oblique ramp development at an obliquely collided irregular margin: geometry and kinematics of the NW Taiwan fold-thrust belt. Tectonics 22, 1–16.CrossRefGoogle Scholar
Lacquement, F, Averbuch, O, Mansy, JL, Szaniawski, R and Lewandowski, M (2005) Transpressional deformations at lateral boundaries of propagating thrust-sheets: the example of the Meuse Valley Recess within the Ardennes Variscan fold-and-thrust belt (N France-S Belgium). Journal of Structural Geology 27, 1788–802.CrossRefGoogle Scholar
Lavecchia, G (1985) Il sovrascorrimento dei Monti Sibillini: analisi cinematica e strutturale. Bollettino della Società Geologica Italiana 104, 161–94.Google Scholar
Lickorish, WH, Ford, M, Bürgisser, J and Cobbold, PR (2002) Arcuate thrust systems in sandbox experiments: a comparison to the external arcs of the Western Alps. Bulletin of the Geological Society of America 114, 1089–107.Google Scholar
Lu, G, Marshak, S and Kent, DV (1990) Characteristics of magnetic carriers responsible for Late Paleozoic remagnetization in carbonate strata of the mid-continent, U.S.A. Earth and Planetary Science Letters 102, 351–61.Google Scholar
Lucente, FP and Speranza, F (2001) Belt bending driven by lateral bending of subducting lithospheric slab: geophysical evidences from the Northern Apennines (Italy). Tectonophysics 337, 53–64.CrossRefGoogle Scholar
Macedo, J and Marshak, S (1999) Controls on the geometry of fold-thrust belt salients. Bulletin of the Geological Society of America 111, 1808–22.2.3.CO;2>CrossRefGoogle Scholar
Malinverno, A and Ryan, WBF (1986) Extension in the Tyrrhenian Sea and shortening in the Apennines as result of arc migration driven by sinking of the lithosphere. Tectonics 5, 227–45.CrossRefGoogle Scholar
Marshak, S (1988) Kinematics of orocline and arc formation in thin-skinned orogens. Tectonics 7, 73–86.CrossRefGoogle Scholar
Marshak, S (2004) Salients, recesses, arcs, oroclines, and syntaxes – a review of ideas concerning the formation of map-view curves in fold-thrust belts. AAPG Memoir 82, 131–56.Google Scholar
Marshak, S, Wilkerson, MS and Hsui, AT (1992) Generation of curved fold-thrust belts: insight from simple physical and analytical models. In Thrust Tectonics, pp. 83–92. London: Chapman & Hall.CrossRefGoogle Scholar
Marton, P and D’Andrea, M (1992) Paleomagnetically inferred rotations of the Abruzzi and Northwestern Umbria. Tectonophysics 202, 43–53.CrossRefGoogle Scholar
Mattei, M, Funiciello, R and Kissel, C (1995) Paleomagnetic and structural evidence for Neogene block rotations in the Central Apennines, Italy. Journal of Geophysical Research 100, 863–83.CrossRefGoogle Scholar
Mattei, M, Kissel, C and Funicello, R (1996) No tectonic rotation of the Tuscan Tyrrhenian margin (Italy) since Late Messinian. Journal of Geophysical Research 101, 2835–45.CrossRefGoogle Scholar
McFadden, PL (1990) A new fold test for palaeomagnetic studies. Geophysical Journal International 103, 163–9.CrossRefGoogle Scholar
McFadden, PL and McElhinny, MW (1988) The combined analysis of remagnetization circles and direct observations in palaeomagnetism. Earth and Planetary Science Letters 87, 161–72.CrossRefGoogle Scholar
McFadden, PL and McElhinny, MW (1990) Classification of the reversal test in palaeomagnetism. Geophysical Journal International 103, 725–9.CrossRefGoogle Scholar
Muttoni, G, Argnani, A, Kent, DV, Abrahamsen, N and Cibin, U (1998) Paleomagnetic evidence for Neogene tectonic rotations in the northern Apennines, Italy. Earth and Planetary Science Letters 154, 25–40.CrossRefGoogle Scholar
Muttoni, G, Garzanti, E, Alfonsi, L, Cirilli, S, Germani, D and Lowrie, W (2001) Motion of Africa and Adria since the Permian: paleomagnetic and paleoclimatic constraints from northern Libya. Earth and Planetary Science Letters 192, 159–74.CrossRefGoogle Scholar
Pace, P and Calamita, F (2014) Push-up inversion structures v. Fault-bend reactivation anticlines along oblique thrust ramps: examples from the Apennines fold-and-thrust belt (Italy). Journal of the Geological Society 171, 227–38.CrossRefGoogle Scholar
Pace, P and Calamita, F (2015) Coalescence of fault-bend and fault-propagation folding in curved thrust systems: an insight from the Central Apennines, Italy. Terra Nova 27, 175–83.CrossRefGoogle Scholar
Pace, P, Pasqui, V, Tavarnelli, E and Calamita, F (2017) Foreland-directed gravitational collapse along curved thrust fronts: insights from a minor thrust-related shear zone in the Umbria-Marche belt, central-northern Italy. Geological Magazine 154, 381–92.CrossRefGoogle Scholar
Pastor-Galán, D, Gutiérrez-Alonso, G, Mulchrone, KF and Huerta, P (2012) Conical folding in the core of an orocline. A geometric analysis from the Cantabrian Arc (Variscan Belt of NW Iberia). Journal of Structural Geology 39, 210–23.CrossRefGoogle Scholar
Pastor-Galán, D, Mulchrone, KF, Koymans, MR, van Hinsbergen, DJJ and Langereis, CG (2017) Bootstrapped total least squares orocline test: a robust method to quantify vertical-axis rotation patterns in orogens, with examples from the Cantabrian and Aegean oroclines. Lithosphere 9, 499–511.CrossRefGoogle Scholar
Pueyo, EL, Pocoví, A., Parés, JM, Millán, H and Larrasoana, JC (2003) Thrust ramp geometry and spurious rotations of paleomagnetic vectors. Studia Geophysica et Geodaetica 47, 331–57.CrossRefGoogle Scholar
Pueyo, EL, Sussman, AJ, Oliva-Urcia, B and Cifelli, F (2016) Palaeomagnetism in fold and thrust belts: use with caution. In Palaeomagnetism in Fold and Thrust Belts: New Perspectives (eds Pueyo, EL, Citelli, F, Sussman, AJ & Olivia-Urci, B), pp. 259–76. Geological Society of London, Special Publication no. 425.Google Scholar
Rodríguez-Pintó, A., Pueyo, EL, Calvín, P, Sánchez, E, Ramajo, J, Casas, AM, Ramón, MJ, Pocoví, A, Barnolas, A and Román, T (2016) Rotational kinematics of a curved fold: the Balzes anticline (Southern Pyrenees). Tectonophysics 677–678, 171–89.CrossRefGoogle Scholar
Santantonio, M (1993) Facies associations and evolution of pelagic carbonate platform/basin systems: examples from the Italian Jurassic. Sedimentology 40, 1039–67.CrossRefGoogle Scholar
Satolli, S, Besse, J and Calamita, F (2008) Paleomagnetism of Aptian-Albian sections from the Northern Apennines (Italy): implications for the 150-100 Ma apparent polar wander of Adria and Africa. Earth and Planetary Science Letters 276, 115–28.CrossRefGoogle Scholar
Satolli, S, Besse, J, Speranza, F and Calamita, F (2007) The 125-150 Ma high-resolution Apparent Polar Wander Path for Adria from magnetostratigraphic sections in Umbria-Marche (Northern Apennines, Italy): timing and duration of the global Jurassic-Cretaceous hairpin turn. Earth and Planetary Science Letters 257, 329–42.CrossRefGoogle Scholar
Satolli, S and Calamita, F (2008) Differences and similarities between the central and the southern Apennines (Italy): examining the Gran Sasso versus the Matese-Frosolone salients using paleomagnetic, geological, and structural data. Journal of Geophysical Research: Solid Earth 113, B10101. doi: 10.1029/2011JB008292.CrossRefGoogle Scholar
Satolli, S and Calamita, F (2012) Influence of inversion tectonics in the bending of a foreland fold-and-thrust belt: the case of the northern Apennines (Italy). Journal of the Virtual Explorer 43, paper 5. 10.3809/jvirtex.2012.00302.CrossRefGoogle Scholar
Satolli, S, Speranza, F and Calamita, F (2005) Paleomagnetism of the Gran Sasso range salient (central Apennines, Italy): pattern of orogenic rotations due to translation of a massive carbonate indenter. Tectonics 24, TC4019. doi: 10.1029/2004TC001771.CrossRefGoogle Scholar
Satolli, S and Turtù, A (2016) Early Cretaceous magnetostratigraphy of the Salto del Cieco section (Northern Apennines, Italy). Newsletters on Stratigraphy 49, 361–82.CrossRefGoogle Scholar
Scheepers, PJJ and Langereis, CG (1994) Paleomagnetic evidence for counter-clockwise rotations in the Southern Apennines fold-and-thrust belt during the late Pliocene and middle Pleistocene. Tectonophysics 239, 43–59.CrossRefGoogle Scholar
Scisciani, V, Agostini, S, Calamita, F, Pace, P, Cilli, A, Giori, I and Paltrinieri, W (2014) Positive inversion tectonics in foreland fold-and-thrust belts: a reappraisal of the Umbria-Marche Northern Apennines (Central Italy) by integrating geological and geophysical data. Tectonophysics 637, 218–37.CrossRefGoogle Scholar
Scisciani, V and Montefalcone, R (2006) Coexistence of thin- and thick-skinned tectonics: an example from the Central Apennines, Italy. In Styles of Continental Contraction (eds Mazzoli, S & Butler, RWH), pp. 33–54. Boulder, Colorado: Geological Society of America, Special Papers 414,.Google Scholar
Scisciani, V, Rusciadelli, G and Calamita, F (2000) Faglie normali nell’evoluzione tortoniano-messiniane dei bacini sinorogenici dell’Appennino centrale esterno. Bollettino della Societa Geologica Italiana 119, 715–32.Google Scholar
Scisciani, V, Tavarnelli, E, Calamita, F and Paltrinieri, W (2002) Pre-thrusting normal faults within syn-orogenic basins of the Outer Central Apennines, Italy: implications for Apennine tectonics. Bollettino della Societa Geologica Italiana 1, 295–304.Google Scholar
Smith, B, Aubourg, C, Guézou, JC, Nazari, H, Molinaro, M, Braud, X and Guya, N (2005) Kinematics of a sigmoidal fold and vertical axis rotation in the east of the Zagros-Makran syntaxis (southern Iran): paleomagnetic, magnetic fabric and microtectonic approaches. Tectonophysics 411, 89–109.CrossRefGoogle Scholar
Speranza, F, Maniscalco, R and Grasso, M (2003) Pattern of orogenic rotations in central-eastern Sicily: implications for the timing of spreading in the Tyrrhenian Sea. Journal of the Geological Society, London 160, 183–95.CrossRefGoogle Scholar
Speranza, F, Mattei, M, Naso, G, Di Bucci, D and Corrado, S (1998) Neogene-Quaternary evolution of the central Apennine orogenic system (Italy): a structural and palaeomagnetic approach in the Molise region. Tectonophysics 299, 143–57.CrossRefGoogle Scholar
Speranza, F, Sagnotti, L and Mattei, M (1997) Tectonics of the Umbria-Marche-Romagna Arc (central northern Apennines, Italy): new paleomagnetic constraints. Journal of Geophysical Research B: Solid Earth 102, 3153–66.CrossRefGoogle Scholar
Tarduno, JA, Lowrie, W, Sliter, WV, Bralower, TJ and Heller, F (1992) Reversed polarity characteristic magnetizations in the Albian Contessa section, Umbrian Apennines, Italy: implications for the existence of a mid-Cretaceous mixed polarity interval. Journal of Geophysical Research 97, 241–71.CrossRefGoogle Scholar
Tavarnelli, E (1993) Evidence for fault propagation folding in the Umbria-Marche-Sabina Apennines (Central Italy). Annales Tectonicae 7, 87–99.Google Scholar
Tavarnelli, E (1997) Structural evolution of a foreland fold-and-thrust belt: the Umbria-Marche Apennines, Italy. Journal of Structural Geology 19, 523–34.CrossRefGoogle Scholar
Tavarnelli, E, Butler, RWH, Decandia, FA, Calamita, F, Alvarez, W and Renda, P (2004) Implications of fault reactivation and structural inheritance in the Cenozoic tectonic evolution of Italy. In The Geology of Italy (eds Crescenti, U, D’Offizi, S., Merlino, S & Sacchi, L), pp. 209–22. Florence: Italian Geological Society.Google Scholar
Thébault, E, Finlay, CC, Beggan, CD, Alken, P, Aubert, J, Barrois, O, Bertrand, F, Bondar, T, Boness, A, Brocco, L, Canet, E, Chambodut, A, Chulliat, A, Coïsson, P, Civet, F, Du, A, Fournier, A, Fratter, I, Gillet, N, Hamilton, B, Hamoudi, M, Hulot, G, Jager, T, Korte, M, Kuang, W, Lalanne, X, Langlais, B, Léger, JM, Lesur, V, Lowes, FJ, Macmillan, S, Mandea, M, Manoj, C, Maus, S, Olsen, N, Petrov, V, Ridley, V, Rother, M, Sabaka, TJ, Saturnino, D, Schachtschneider, R, Sirol, O, Tangborn, A, Thomson, A, Tøffner-Clausen, L, Vigneron, P, Wardinski, I and Zvereva, T (2015) International geomagnetic reference field: the 12th generation. Earth, Planets and Space 67, 79. doi: 10.1186/s40623-015-0228-9.CrossRefGoogle Scholar
Tozer, RSJ, Butler, RWH and Corrado, S (2002) Comparing thin- and thick-skinned thrust tectonic models of the Central Apennines, Italy. Stephan Mueller Special Publication Series 1, 181–94.CrossRefGoogle Scholar
Turtù, A., Satolli, S, Maniscalco, R, Calamita, F and Speranza, F (2013) Understanding progressive-arc- and strike-slip-related rotations in curve-shaped orogenic belts: the case of the Olevano-Antrodoco-Sibillini thrust (Northern Apennines, Italy). Journal of Geophysical Research: Solid Earth 118, 459–73.Google Scholar
Van der Voo, R (1990) The reliability of paleomagnetic data. Tectonophysics 184, 1–9.CrossRefGoogle Scholar
Van der Voo, R (1993) Paleomagnetism of the Atlantic, Tethys and Iapetus Oceans. Cambridge: Cambridge University Press, 411 pp.CrossRefGoogle Scholar
Weil, AB and Sussman, AJ (2004) Classifying curved orogens based on timing relationships between structural development and vertical-axis rotations. In Orogenic Curvature: Integrating Paleomagnetic and Structural Analyses (eds Sussman, AJ & Weil, AB), pp. 1–15. Boulder, Colorado: Geological Society of America, Special Paper 383.Google Scholar
Weil, AB, Yonkee, A and Sussman, A (2010) Reconstructing the kinematic evolution of curved mountain belts: a paleomagnetic study of Triassic red beds from the Wyoming salient, Sevier thrust belt, U.S.A. Bulletin of the Geological Society of America 122, 24–49.CrossRefGoogle Scholar
Zijderveld, JDA (1967) A.C. demagnetization of rocks: analysis of results. In Methods in Palaeomagnetism (eds Collinson, DW, Creer, KM & Runcorn, SK), pp. 254–86. Amsterdam: Elsevier.Google Scholar