Morphotectonics of the Upper Tiber Valley (Northern Apennines, Italy) through quantitative analysis of drainage and landforms
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  • 作者:L. Melelli (1)
    S. Pucci (2)
    L. Saccucci (3)
    F. Mirabella (1) (4)
    F. Pazzaglia (5)
    M. Barchi (1)

    1. Dipartimento di Fisica e Geologia
    ; Universit脿 di Perugia ; Perugia ; Italy
    2. Istituto Nazionale di Geofisica e Vulcanologia
    ; Rome ; Italy
    3. Perugia
    ; Italy
    4. Istituto di Ricerca per la Protezione Idrogeologica
    ; Consiglio Nazionale delle Ricerche ; via Madonna Alta 126 ; 06128 ; Perugia ; Italy
    5. IntGeoMod s.r.l.
    ; Via Innamorati 7/a ; 06123 ; Perugia ; Italy
  • 关键词:Geomorphometry ; Neotectonic ; Tiber basin ; Umbria region
  • 刊名:Rendiconti Lincei
  • 出版年:2014
  • 出版时间:December 2014
  • 年:2014
  • 卷:25
  • 期:2-supp
  • 页码:129-138
  • 全文大小:3,525 KB
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    12. Ciotoli, G, Della Seta, M, Monte, M, Fredi, P, Lombardi, S, Lupia Palmieri, E, Pugliese, F (2003) Morphological and geochemical evidence of neotectonics in the volcanic area of Monti Vulsini (Latium, Italy). Quatern Int 101鈥?02: pp. 103-113 CrossRef
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    15. D鈥橝gostino, N, Jackson, J, Dramis, F, Funicello, R (2001) Interaction between mantle upwelling, drainage evolution and active normal faulting: an example from the central Apennines (Italy). Geophys J Int 147: pp. 475-497 CrossRef
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    23. Melelli L, Saccucci L, Fiorucci L, Barchi M, Mirabella F, Pazzaglia F, Pucci S (2012) Geomorphological quantitative analysis of high Tiber Valley drainage network (Umbria, Italy). Rend Online Soc Geol It 21, parte II, 1120鈥?121
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    26. Pucci S, Mirabella F, Pazzaglia F, Barchi MR, Melelli L, Tuccimei P, Soligo M, Saccucci L (2014) Interaction between regional and local tectonic forcing along a complex quaternary extensional basin: Upper Tiber Valley, Northern Apennines, Italy. Quat Sci Rev 102:111鈥?32. doi:10.1016/j.quascirev.2014.08.009
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  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Life Sciences
    Biomedicine
    History of Science
  • 出版者:Springer Milan
  • ISSN:1720-0776
文摘
We present a geomorphological analysis of the recent extensional tectonics of a Quaternary continental basin in the Northern Apennines (Italy). The study area is focused on Upper Tiber Valley (UTV), a basin elongated for 70 km in NNW-SSE direction hosting the Tiber River. The area is characterized by a series of features that make it an excellent case study: (i) homogeneity of lithology (ii) active faults, and (iii) strong morphogenetic activity. In this study, 36 hydrographical basins, tributaries of Tiber River, have been analysed. A preliminary qualitative geomorphological setting was outlined pointing out that the drainage river network shows meaningful evidence of tectonic control, such as abrupt changes in stream directions, knickpoints and steepness anomalies alignments along meaningful length in adjacent basins. Besides, the tectonic control is well marked in base level changes and consequent tectonically induced downcutting. Signs of neotectonics are highlighted by structural landforms too. The entrenchment of alluvial fans, the triangular facets and the fault planes are mapped by field survey and aerial photo interpretation. In addition, a quantitative analysis was also performed. Linear, areal and volumetric indexes related to drainage basins and river networks are taken into account. The geometry of the escarpments delimiting the basin and the landforms detected along the adjacent piedmont are investigated. The ranges of values, according to the existing literature, confirm a condition of wide-ranging morphological disturbance. In the central part of the study area, while the western basins are almost in equilibrium, the eastern ones reveal clear signs of disequilibrium, this is particularly evident along the distal segment of the river network. These data, joined with the characteristics of the escarpment and piedmont junction, confirm that the neotectonic activity, in the centre and in the eastern side of the basin, is the main factor controlling the morphological system.

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