We investigate crustal deformation within the upper plate of Ionian Subduction Zone (ISZ) at different time scales by (i) refining geodetic rates extension from continuous Global Navigation Satellite System (GNSS) measurements and (ii) mapping sequence Late Quaternary raised marine terraces tectonically deformed West Crati normal fault, in northern Calabria. This region experienced damaging ear...

Abstract The Matano fault in central Sulawesi is one of the major strike-slip faults that accommodate rapid left-lateral slip between Pacific and Australian plates. has a high seismic potential producing large (M w ≥7) earthquakes. However, was less studied, unlike Palu-Koro fault. This paper presents preliminary results our active investigation eastern which may help understanding neotectonics...

We analyzed the tectonics and stratigraphy of Southern Great Tarakan Basin to determine its tectonic evolution during Mesozoic-Cenozoic Eras, basin geometry, potential hydrocarbon using integrated surface subsurface data. can be divided into three sub-basins, Berau, Muara, South Tarakan. They comprise deposits Jurassic Quaternary age, which assigned five mega sequences based on their lithologic...

The Barkol Tagh and Karlik Tagh ranges of the easternmost Tien Shan are a natural laboratory for studying the fault architecture of an active termination zone of a major intracontinental mountain range. Barkol and Karlik Tagh and lesser ranges to the north are bounded by active thrust faults that locally deform Quaternary sediments. Major thrusts in Karlik Tagh connect along strike to the east ...

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 ...