Structural control on badland slope evolution: A case study from the southern Apennines (Italy)

被引:7
|
作者
Bentivenga, M. [1 ]
Agosta, F. [1 ,2 ]
Palladino, G. [3 ]
Piccarreta, M. [4 ]
Prosser, G. [1 ]
机构
[1] Univ Basilicata, Dipartimento Sci, I-85100 Potenza, Italy
[2] Geosmart Italia, Basilicate, Italy
[3] Univ Aberdeen, Sch Geosci, Dept Geol & Geophys, Aberdeen, Scotland
[4] Minist Pubbl Istruz, Rome, Italy
关键词
Badland evolution; Riedel fractures; Clay deformation; Fault zones; Southern Italy; UPPER ORCIA VALLEY; MONTE ALPI; PISTICCI BASILICATA; EROSION PROCESSES; PIGGYBACK BASIN; THRUST-BELT; AREA; TUSCANY; PLEISTOCENE; TECTONICS;
D O I
10.1016/j.geomorph.2020.107518
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
This work focuses on a multi-method study of badlands exposed in two different areas of southern Italy. Results of both geomorphological and structural geological studies are obtained by combining field and laboratory analyses of the badlands affecting Plio-Quaternary silty-clays of southern Italy. Results are discussed in terms of deformation mechanisms and badland formation and evolution. Results highlight the role played by pre-existing structural heterogeneities, such as high-angle faults and joints, on both gravitational processes and water circulation. The aforementioned heterogeneities are due to specific tectonic stress regimes, and are interpreted in light of their genetic nature, kinematics, attitude, geometry, relative timing of formation, and aerial distribution. Results of this work are summarized in a four-stage conceptual model characterized by specific genetic mechanisms. The conceptual model includes representative sketches aimed at assessing the time-dependant evolution of the badlands. A profound link between structural geology and geormophological processes is therefore envisioned for the badlands of southern Italy. (C) 2020 Elsevier B.V. All rights reserved.
引用
收藏
页数:18
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