Velocity structure above seismological bedrock estimated from earthquake recordings: an application of diffuse wave-field concept to strong motions in Iran

Earth, Planets and Space

Table 1 The strong motion stations of this study

Station	Latitude	Longitude	Province/prefecture	Sensor depth (m)	Surface geology^a
KRD	34.2802	46.2408	Kermanshah	Z = 0	Q^t2: Quaternary young alluvial terrace
SLS	34.7432	46.1505			Q^t: Quaternary fan and alluvial plain
SPZ	34.4554	45.8699			Qt: Quaternary coarse and fine grain alluvium Bk: Pliocene thin bedded to massive consolidated conglomerate, Bakhtyari formation
IBRH11	36.3701	140.1401	Ibarakiken	Z = 0, 103	a: Quaternary, Holocene gravel, sand and mud alluvium Sk: Quaternary, Middle Pleistocene gravel, sand and mud, Sakaibayashi formation

^aThe reference is either Geological Survey and Mineral Exploration of Iran or Geological Survey of Japan