Abstract The deformation pattern and slip partitioning related to oblique underthrusting of the Tarim Basin in eastern Tian Shan orogenic belt are not well understood because interior images lacking. Baoertu fault is an E-W–striking, ~350-km-long reactivated basement structure within Shan. In this study, we quantify its late Quaternary activity based on interpretations detailed high-resolution ...

one of the methods for the determination of focal mechanisms of earthquakes is the linear inversion of moment tensor in time domain. that method is used here for determining of the focal mechanisms the darbe astaneh silakhor earthquake of 31 march 2006 and two of its foreshocks and six aftershocks with local magnitude more than 4. the data of six broadband stations of the international institut...

Varying estimates of both present-day strain accumulation and long-term slip rate on the Doruneh left-lateral strike-slip fault, NE Iran, have led to suggestions that it exhibits large along-strike and/or temporal changes in activity. In this study, we make compare measured using geodesy geomorphology, spanning time periods ranging from decadal 100 ka. To image strain, process 7 years (2003–201...

A variety of tectonic processes spread along the circum-Mediterranean orogenic belts driven by convergence major plates, episodes slab retreat and lateral vertical mantle flows. Here, we provide an updated view crustal stress strain-rate fields for Albanides belt in eastern Adria-Eurasia boundary. We framed a new geodetic-based source model 2019 Mw6.4 Durrёs earthquake light regional deformatio...

Abstract Topography along strike‐slip fault restraining bends is theoretically self‐limited by erosion, block translation and the expected abandonment of bends. However, Denali (6,194 m) Foraker (5,304 are located within a bend dextral Fault system. We reveal role evolution in mountain building with physical experiments scaled to simulate Alaska Mount McKinley (MMRB). Despite natural complexity...

Abstract. The Dinaric Fault System in western Slovenia, consisting of NW–SE-trending, right-lateral strike-slip faults, accommodates the northward motion Adria with respect to Eurasia. These active faults show a clear imprint morphology, and some them hosted moderate instrumental earthquakes. However, it is largely unknown if also had strong earthquakes late Quaternary. This hampers our underst...

The so-called Pelusium Megashear System (PMS), consists of echelon left-lateral megashears crossing Africa from the Nile-Delta since the Precambrian times. Although this system is questioned by some scientists, its existence is supported by others. This research work provides evidences for the existence of the PMS near Egypt’s capital (Cairo city). Evidence is interpreted from gravity, magnetic...

High-resolution magnetotelluric and gravity data have been collected over the Kiejo-Mbaka geothermal field, located along NW–SE trending Mabka fault, in Karonga Rift basin (East Africa System). Such resolution allowed to reconstruct field structure with unprecedented detail. Resistivity modelling has obtained by three-dimensional finite-differences inversion of MT data, while density accomplish...

Based on the interpretation of 2D seismic profiles integrated with surface geological investigations, a mechanism responsible for formation large scale normal fault zone has been proposed. The fault, here referred to as Rycerka Fault, predominantly dip-slip component detachment located at base Carpathian units. developed due an anticlinal stack within Dukla Unit overlain by Magura Units. Stacki...

With the increasing demand for higher performance, safety and reliability of dynamic systems, fault diagnosis has received more and more attention. The observer-based strategy is one of the active research fields, which is widely used to construct model-based fault detection systems for technical processes which can be well modelled as linear time invariant systems. Fault diagnosis for nonlinea...