Since their development in the 1960s, seismic arrays have given a new impulse to
seismology. Recordings from many uniform seismometers in a well‐defined, closely spaced …

Seismic tomography has been a vital tool in probing the Earth's internal structure and
enhancing our knowledge of dynamical processes in the Earth's crust and mantle. While …

Seismic interferometry is an exciting new field in geophysics utilizing multiple scattering
events to provide unprecedented views of the Earth's subsurface. This is the first book to …

Claerbout's daylight imaging concept is generalized to a theory of interferometric seismic
imaging (II). Interferometric seismic imaging is defined to be any algorithm that inverts …

We use common conversion point (CCP) stacking of Ps receiver functions to image the
crustal structure and Moho of the Garhwal Himalaya of India. Our seismic array of 21 …

Crustal and upper-mantle seismic discontinuities beneath eastern Turkey are imaged using
teleseismic S-to-P converted phases. Three crustal phases are observed: the Moho with …

This paper provides a review of array-based imaging techniques that use converted and
scattered teleseismic waves. It addresses various aspects of the imaging process, from the …

This is the first paper in a three‐part series that examines formal inversion of the teleseismic
P wave coda for discontinuous variations in elastic properties beneath dense, three …

An oceanic plateau, the Yakutat terrane, has entered the subduction system across
southcentral Alaska. Its down‐dip fate and relationship to overlying volcanism is still …

Seismic arrays, first introduced in the late 1950s to detect underground nuclear explosions,
have helped to improve our knowledge about the structure of the Earth for the last 40 years …