Applications for the Roer Valley Graben and coal mine induced displacements in the southern Netherlands Improving radar interferometry for monitoring fault-related surface deformation. Applications for the Roer Valley Graben and coal mine induced displacements in the southern Netherlands Miguel Caro Cuenca Publications on Geodesy 81

[1] Several zones of graben (Memnonia, Sirenum, Icaria, Thaumasia, and Claritas Fossae) extend radially away from the Tharsis rise in the southern hemisphere of Mars for distances of up to 3000–4000 km. These graben systems are commonly interpreted to be related to regional tectonic deformation of the Tharsis rise associated with either upwelling or loading. We explore the possibility that thes...

Abstract The Central Graben is a Mesozoic sedimentary basin that significantly influenced by rift and salt tectonics. Its southern part located in the German Dutch sectors of North Sea. Even though studies exist on tectonic stratigraphic development Danish Graben, as an important link less investigated. We aim to fill this gap investigate from Latest Triassic Early Cretaceous, relative influenc...

We describe the morphology of a large and complex graben structure in the western Thauma-sia region (the " Thaumasia graben " [1] or TG). We consider possible fault geometries, determine extension , and discuss shortly possible models for its origin. Background: Situated at the western border of the Thaumasia plateau, the TG is one of the most prominent fault-bounded structures on Mars. It is ~...

The Szamotuly Graben covers the southernmost part of Permo-Mesozoic Poznan–Szamotuly Fault Zone. Along this regional discontinuity there are several salt structures, including diapir, over which an extensional graben formed in Paleogene and Neogene. is located north Poznan central-western Poland, NW–SE-trending, ~20 km long, 3–5.5 wide, up to 160 m deep. It filled with Lower Oligocene Neogene s...

The inversion technique of Nowack and Lutter (1988a) and Lutter et al. (1990) has been applied to first arrival seismic refraction data collected along Line A of the 1986 Lake Superior GLIMPCE experiment, permitting comparison of the inversion image with an independently derived forward model (Trehu et al., 1991; Shay and Trehu, in press). For this study, the inversion method was expanded to al...

This study presents a seismotectonic analysis of the Miocene-aged Hegau-Bodensee Graben, major tectonic element in northern foreland European Central Alps. The graben is characterized by comparatively low strain rates and low-to-moderate seismicity. Our builds on seismological earthquakes recorded recently densified seismometer network. derived high-precision absolute relative hypocenter reloca...

The Lower Cretaceous Tuxen (lower Hauterivian – upper Barremian) and Sola (upper Barremian Albian) Formations in the Danish Central Graben (North Sea) constitute one of oldest chalk successions recorded globally, but have received little attention with regards to sedimentary facies depositional processes. This study presents first comprehensive carbonate analysis succession, retrieved from seve...