The Cenozoic history of the retreating Hellenic subduction system in the eastern
Mediterranean involves subduction, accretion, arc magmatism, exhumation, normal faulting …

We study the upper mantle P wave velocity structure below the Euro‐Mediterranean area,
down to 1000 km depth, by seismic travel time tomography. We invert summary residuals …

The tectonic history of the western Tethys since the Late Triassic is illustrated through a set
of computer-generated plate reconstructions, which are based on a rigorous plate motions …

We present results from a combined multichannel seismic reflection (MCS) and wideangle
onshore/offshore seismic experiment conducted in 1996 across the southeast Greenland …

In this paper, we discuss the possibility that the North Anatolian fault (NAF) results from the
deep deformation of the slab beneath the Bitlis–Hellenic subduction zone. We described the …

Seismic data represent one of the most valuable resources for investigating the internal
structure and composition of the earth. One of the first people to deduce earth structure from …

The prevailing idea for the geologic evolution of the western Mediterranean in the Cenozoic
is based on north dipping subduction near the gulf of Lyon undergoing vigorous rollback …

The Sichuan‐Yunnan region in southwest China is located in the boundary area between
the active Tibetan Plateau to the west and the stable South China platform to the east. This …

Recent advances in global imaging have lead to tomographic mantle models with regional
scale details. To improve these models further, we have extended the usual linearized …

Accurate locations of 961 shallow and intermediate depth earthquakes, which occurred
between 1956 and 1995 in the Hellenic arc (34–39° N, 19–28° E), are used to define the …