we focus on the exhumed damage zones of strike-slip faults dissecting the south-western part of the Mesozoic cover of the Late Palaeozoic Holy Cross Mountains Fold Belt (HCFB) in Poland (Fig.1a–c) (e.g. Czarnocki1938; Mastella and Konon2002). We study the damage zones having...
10 Simplified time–space diagram of small-scale sequence 13 and its interpreted 5 elementary sequences, outlining correlatable and non-correlatable intervals in the studied sections. SB: sequence boundary; MFS: maximum-flooding surface; Ru: Rusel; Ma: March- airuz; SC: St. Claude; La: La...
The problem of earthquakes represents a significant issue for a large territory of Kazakhstan and requires to be studied carefully. The introduction of the European code of practice in Kazakhstan contributed to the need for international design methods to increase the designed buildings’ safety. Even...
Using borehole core analysis to reveal Late Quaternary paleoearthquakes along the Nankou-Sunhe Fault, Beijing. Sci. China Ser D Earth Sci. 2008, 51, 1154–1168. [Google Scholar] [CrossRef] Huang, M.; Ninic, J.; Zhang, Q. BIM, machine learning and computer vision techniques in ...
Seismic Performance of a Non-Structural Component with Two Supports in Bidirectional Earthquakes Considering Soil-Structure Interaction; Seismic Performance of Soil-Foundation-Structure Systems; CRC Press: Boca Raton, FL, USA, 2017; pp. 73–80. [Google Scholar] Martakis, P.; Taeseri, D.; Chatzi...
[10,11], are available everywhere. These networks can be potentially used as a large seismic array for survey and monitoring purposes. Surface waves can be generated by a variety of sources, including earthquakes, explosions, and vibrations from human activities such as traffic and construction. ...
Innovations in (U-Th)/He, fission-track, and trapped-charge thermochronometry with applications to earthquakes, weathering, surface-mantle connections, and the growth and decay of mountains. Tectonics 2019, 38, 3705–3739. [CrossRef] 15. Ehlers, T.A.; Farley, K.A. Apatite (U+Th)/He ...
Earthquake - Shallow, Intermediate, Deep Foci: Most parts of the world experience at least occasional shallow earthquakes—those that originate within 60 km (40 miles) of the Earth’s outer surface. In fact, the great majority of earthquake foci are shal