Struttura, esumazione ed evoluzione morfologica del nucleo mesozoico del Monte Motola (Cilento, Italia meridionale)

Bollettino- Societa Geologica Italiana (Impact Factor: 1). 01/2008; 127(3):477-493.

ABSTRACT Il Monte Motola è un rilievo formato da carbonati di mare basso prevalentemente mesozoici e circondato da un'aureola di terreni argillosi e calcareo-marnosi più facilmente erodibili e tormentati da un diffuso dissesto. È posto a cavallo della porzione più interna del promontorio del Cilento (Campania, Italia meridionale) e della depressione del Vallo di Diano ed è perimetrato da un complesso sistema di faglie transpressive ed estensionali certamente attive in tempi plio-quaternari che, unitamente all'azione erosiva del reticolo idrografico, hanno consentito l'esumazione del nucleo mesozoico del rilievo. Lo studio morfotettonico ha permesso di stimare a circa 0.6 mm/a il tasso medio di sollevamento della struttura durante il Quaternario, in buon accordo con quanto noto per la zona assiale dell'Appennino meridionale. L'area del Monte Motola si è rivelata una zona di concentrazione della deformazione nel contesto della transpressione tardo-pliocenica operante su un'area ben più vasta dell'Appennino meridionale, e tale sembra essere rimasta anche nella successione dei regimi deformativi quaternari. Tale peculiarità appare ereditata dallo scenario paleogeografico mesozoico in cui l'elemento corrispondente all'attuale dorsale del Monte Motola-Monte Vivo doveva già rappresentare un moderato alto strutturale, capace tuttavia di generare condizioni di anisotropia atte a condizionare l'intera storia tettono-evolutiva dell'area.

ABSTRACT: Geology, geomorphology, and exhumation modalities of the Monte Motola structure, Cilento region, southern Italy. Southern Italy underwent a poly-phase tectonic history from late Oligocene to Quaternary times, after the positive inversion of the Apulian segment of the African Mesozoic passive margin. «External» structural units derived from this important palaeogeographic domain and their deformation started in the early Miocene, when the Liguride ophiolite-bearing accretionary prism and the Sicilide Complex (i.e. the assemblage of the «Internal units») overthrust the westernmost portion of the continental margin. This was articulated in a series of platforms and basins where also more restricted palaogeographic elements, such as emerged zones of a platform, structural highs, seamounts and narrow troughs, were present in different times. Monte Motola is a sharp and narrow positive morphostructure made of Mesozoic shallow-water carbonates surrounded by Cretaceous to Miocene «internal» clayey units, largely affected by landslides. This area is located in the inner part of the Cilento promontory and bordered to the east by the Quaternary intermontane basin of the Vallo di Diano. Although Monte Motola has lithology and elevations similar to the calcareous massifs located to the
north (Alburni Mts) and to the south (Mt. Cervati), it is morphologically separated from the other mountains by two narrow troughs in which shaly and marly units crop outs, forming a contrasting soft landscape. The calcareous ridge of Monte Motola-Monte Vivo is in fact completely bordered by upper Pliocene to Quaternary transpressional and extensional faults that – together with the activity of the fluvial net – allowed the exhumation of its Mesozoic core. The progressive lateral migration of part of an ancient hydrographic network, expressed by a meandered and weakly intrenched stream and marked by several other relics of fluvial channels, related to the organization of erosional land surfaces in different orders as the erosion base level changed, allowed to reconstruct the
main steps of exhumation and morphological evolution of the ridge and to calculate the uplift/erosion rates during the last 2.5 Ma. The mean value is ca. 0.6 mm/a, in good agreement with those calculated in previous contributions for the axial zone of the southern Apennines. This study also revealed that Monte Motola is a zone of strain
concentration in the context of the late Pliocene transpression which affected a lager sector of the southern Apennines. Quaternary tectonics inherited such a peculiarity, by amplifying the uplift and the separation of the mountain by the rest of the relief. The anisotropy acquired during Cretaceous times and caused by palaeotectonic extensional faulting seems to be the reason for the differential behaviour of the study area with respect to the adjacent massifs. Indeed, in the Mesozoic palaeogeographic scenario Monte Motola
could have represented a minor structural high bordered by normal (or transtensional) faults, probably characterized by moderate offsets but yet able to generate a textural grain that since influenced the successive local tectonic history.

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    ABSTRACT: The geomorphological evolution of the Pliocene-Quaternary Auletta basin, a wide fault-bounded depression of the southern Apennines axial zone, Italy, was reconstructed using both DEM-based morphometric analysis and classical morphotectonic investigations. Morphotectonic analyses have been integrated with geological, structural and paleomagnetic data in order to reconstruct the Quaternary evolution of the area.The Auletta basin coincides with the lower valley of the Tanagro River and is filled by Pliocene to Pleistocene marine and continental sediments. The strike of the basin is N120-130°, according to the main fault systems of the area.Long-term landscape evolution results from interaction and feedback of geomorphic stages with the morphogenesis of erosional land surfaces alternating with tectonic pulses in which also block-tectonic rotation occurred. The ages of the morphological de-activation of such terraced surfaces have been roughly defined on the grounds of their morpho-stratigraphic relationships with Pliocene and Quaternary deposits, and better constrained by radiometric dating. Tectonic tilting has been established from morphological relationships between rotated blocks related to the activity of the Alburni fault line and the several generations of erosional and depositional land surfaces. The stratigraphic, structural, paleomagnetic and geomorphological data presented here suggest that the studied basin appears to have a more complex tectonic evolution than an extensional graben. Transtensional tectonics along NW-SE striking, listric faults of the Alburni margin system created the depression since Pliocene times, whereas extensional tectonics plays a key role in the middle to late Pleistocene morphotectonic evolution of the basin. This work demonstrates the usefulness of an integrated analysis in order to extract information on tectonic activity and landscape evolution in the Auletta basin, as an example for other study areas. © 2011 Elsevier B.V.
    Geomorphology 11/2011; 134(3-4-3-4):326-343. DOI:10.1016/j.geomorph.2011.07.009 · 2.58 Impact Factor
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    ABSTRACT: The opening kinematics of several Pliocene to Quaternary tectonically controlled continental basins scattered along the axis of the southern Italian Apennines and their morphological features and evolution have been compared to define the behaviour of this particular interconnected negative morphostructure. In particular, three different but morphologically connected intermontane basins have been here investigated from a morphotectonic point of view (from the north: Auletta, Vallo di Diano, and Sanza basins). They are filled by more or less thick marine and/or continental sequences of sediments, Pliocene to Quaternary in age. Such basins are shaped by erosional land surfaces and fluvial dissection. The ages of the morphological de-activation of the terraced surfaces have been roughly defined on the basis of their morpho-stratigraphic relationships with Pliocene and Quaternary deposits, and better constrained by radiometric dating. The NNW-SSE-trending fault of the Alburni Mts, bordering the Auletta basin, indicates former left-lateral transtensional kinematics and later dip-slip kinematics, whereas the N140-150°-striking master fault bounding the Vallo di Diano basin is a normal fault. The Sanza basin can be assimilated to a morphostructural trough coinciding with a long-term transfer zone of the chain, in which a severe change in stress field, uplift rate, climate conditions, and relief production occurred during Pleistocene times. Such a complicated morphostructural setting may be interpreted as a function of the original orientation of the structural depressions, only partially coeval. In this sense, the Vallo di Diano basin should represent the structural low generated by pure extension during the Pleistocene, but probably already living as a Pliocene seaway, whereas both the Auletta and Sanza basins stand for two lateral branches with oblique kinematics, inherited from a pre-existing (i.e. Pliocene in age) set.
    Rendiconti Lincei. Scienze Fisiche e Naturali 12/2014; 25(S2):1-12. DOI:10.1007/s12210-014-0325-x · 0.76 Impact Factor
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