Reply to the comments by G. Bertotti and V. Picotti on: “Uplift and contractional deformation along a segmented strike-slip fault system: the Gargano Promontory, southern Italy”

2004 ◽  
Vol 26 (12) ◽  
pp. 2327-2329 ◽  
Author(s):  
Charles M. Brankman ◽  
Atilla Aydin
2018 ◽  
Author(s):  
Emanuela Falcucci ◽  
Maria Eliana Poli ◽  
Fabrizio Galadini ◽  
Giancarlo Scardia ◽  
Giovanni Paiero ◽  
...  

Abstract. We investigated the eastern corner of northeastern Italy, where the NW-SE trending dextral strike-slip fault systems of western Slovenia intersects the south-verging fold and thrust belt of the eastern Southern Alps . The area suffered the largest earthquakes of the region, among which are the 1511 (Mw 6.3) event and the two major shocks of the 1976 seismic sequence, with Mw = 6.4 and 6.1 respectively. The Colle Villano thrust and the Borgo Faris-Cividale strike-slip fault have been first analyzed by interpreting industrial seismic lines and then by performing morpho-tectonic and paleoseismological analyses. These different datasets indicate that the two structures define an active, coherent transpressive fault system that activated twice in the past two millennia, with the last event occurring around the 15th–17th century. The chronological information, and the location of the investigated fault system suggest its activation during the 1511 earthquake.


Geology ◽  
2004 ◽  
Vol 32 (10) ◽  
pp. 837 ◽  
Author(s):  
Charles K. Wilson ◽  
Craig H. Jones ◽  
Peter Molnar ◽  
Anne F. Sheehan ◽  
Oliver S. Boyd

1998 ◽  
Vol 145 (1-2) ◽  
pp. 105-114 ◽  
Author(s):  
Philippe Muchez ◽  
Manuel Sintubin

Sign in / Sign up

Export Citation Format

Share Document