Publisher Summary This chapter focuses on the methodology for determining whether
observed sediment deformation had a seismic shaking or a nonseismic origin. The chapter …

As iron‐bearing minerals—ferrimagnetic minerals in particular—are sensitive to stress,
temperature, and presence of fluids in fault zones, their magnetic properties provide …

There has been a lively debate since the 1980s on distinguishing between paleo-tsunami
deposits and paleo-cyclone deposits using sedimentological criteria. Tsunami waves not …

Natural CO2 discharges are abundant in Turkey as evident from ongoing deposition of
recent terrace-mound travertines and emplacement of significant travertine vein and breccia …

Soft-sediment deformation structures associated with slumps and mass transport deposits
(MTDs) are generally considered to form at the surface when unlithified sediment moves …

Abstract The Dead Sea rift offers a wealth of information about pre-instrumental
earthquakes. The types of potential archives include historic seismicity, archaeological sites …

The irregular distribution of sand injections, traditionally termed “dykes” in the Polish
geological literature, within individual Carpathian units and within individual lithofacies were …

Fold duplexes transfer displacement from a lower to an upper bounding detachment system
via trains of folds with broadly parallel geometries. While they have been previously …

Rectangular drainage networks are characterized by right‐angle bends and confluences.
The formation of such drainage patterns is commonly associated with orthogonal sets of …

Abstract The Dadaepo Basin is a small Late Cretaceous sedimentary basin in SE Korea,
located on the eastern margin of Asia. The basin is an isolated extensional basin situated …