Results 81 to 90 of about 7,206 (227)
Abstract We use an innovative geophysical approach to reconstruct the deep structure of Campo Felice, an important extensional basin in the central Apennines (Italy) where active crustal extension is accommodated by normal faults capable of generating earthquakes of magnitude MW 6+.
V. Sapia +23 more
wiley +1 more source
The Role of Co‐Seismic Devolatilization in Driving Aftershock Sequences in Greece
Abstract We investigate the role of co‐seismic devolatilization in driving aftershock sequences, focusing on three recent sequences in Greece: Thiva, Damasi, and Florina. We use a numerical model incorporating non‐linear diffusion with a source term that accounts for fluid generation via thermal decomposition of carbonates.
Gaëlle Toussaint +3 more
wiley +1 more source
Flexural deformation of the continental lithosphere [PDF]
Prior work focused primarily on the Adriatic and northern Ionian regions. The results of these studies have been summarized previously, and so are only briefly discussed.
core +1 more source
Tectonostratigraphic terranes and zones juxtaposed along the Mid-Hungarian Line: their contrasting evolution and relationships [PDF]
The Mid-Hungarian (or Zagreb-Zemplin) Line of WSW–ENE strike divides the Pannonian basement into two mega-units, the Tisia Composite Terrane in the SE and the ALCAPA Composite Terrane in the NW. They became juxtaposed no earlier than the Middle Miocene
Brezsnyánszky, Károly +4 more
core +1 more source
Abstract Understanding the relationship between surface and deep geological processes in tectonically active settings is crucial for unraveling the factors controlling landscape evolution and topographic growth. Here, we present the first basin‐averaged 10Be‐derived denudation rates for the Albanides, a subduction orogen in the Central Mediterranean ...
C. Bazzucchi +8 more
wiley +1 more source
Gravel bar shielding: A mechanism responsible for bar stability in gravel‐ and cobble‐bedded streams
In this study, we demonstrate that coarse‐grained bar edges, referred to as “lateral lag deposits”, play a key role in stabilizing non‐vegetated gravel‐cobble bars, particularly during lower‐discharge flooding events. We also describe the morphology of these gravel‐bar structures in a braided‐wandering stream.
Ariel do Prado +6 more
wiley +1 more source
Tectono-sedimentary evolution of upper Assam “inter-orogenic” peripheral foreland basin, India
The northern periphery of the Indian craton is the leading edge of the under-thrusting continent in the continent–continent collision set up between the Indian and Eurasian plates.
S. K. Biswas, Gaurav Chauhan
doaj +1 more source
Ophiolitic regions are one of the most complex geology settings. Mapping in these parts need broad and precise studies and tools because of the mixture rocks and confusion units.
Bahram Bahrambeygi, Hesam Moeinzadeh
doaj +1 more source
Geology of Tunceli-Bingöl Region of Eastern Turkey
This region is located in the Taurus orogenic belt of the highland district of Eastern Turkey. Lower Permian metasediments and Upper Permian suberystalline limestone are the oldest exposed formations of this region.
F. A. AFSHAR
doaj
The level of water in aquifers depends mostly on precipitation. However, recent research has shown that greater annual rainfall values do not necessarily trigger off an automatic increase in groundwater recharge. The lowering of the water table may result not only from lower precipitation, but also from intensification in evaporation and a decreased ...
Sebastian Buczyñski, Marek Wcislo
openaire +2 more sources

