Western Fortuna Tessera, Ishtar Terra, records polyphase deformation. Structures include: ribbons forming long, narrow, steep-sided troughs that reflect surface layer extension; N-trending folds related to Maxwell Montes deformation; short, wide, NW-trending graben that reflect late local extension; and, within the southwestern map area, gentle, E-trending warps, which postdate ribbon structure...

In diesem Beitrag stellen wir die Archäologische Sandbox vor: Ein Tangible User Interface (TUI) mit dem archäologische Ausgrabungsstätten und dort gefundene Artefakte exploriert werden können. Das System zielt auf den Einsatz in Museen ab, die ihren Besuchern den Zusammenhang von ausgestellten Exponaten und der Ausgrabungsstätte näherbringen möchten, an der diese gefunden wurden. Den Kern des T...

A program, INV2P5DSB, has been developed to simultaneously estimate the depth of a 2.5-D sedimentary basin and regional background from observed gravity anomalies. The density contrast is assumed to be varying parabolically with depth above the basement interface. The main program is supported with two subroutines GRAV2P5D and SIMEQ and a function GPRM. The analysis of gravity anomalies due to ...

Abstract The 2014–2015 CE rift event associated with the Bárðarbunga eruption at Holuhraun, Iceland, offers a unique opportunity to study spatial and temporal evolution of graben. We present first four-dimensional (three-dimensional plus time) monitoring formation graben during active magma transport using suite digital elevation models spanning from shortly before throughout 6 months up 4.5 ye...

Abstract This article presents the results of an integrated interpretation measurements made using Audio-Magnetotellurics and Seismic Reflection geophysical methods. The obtained were used to build model shallow subsurface cover consisting Cenozoic deposits, which then formed basis for a detailed lithological tectonic deeper Mesozoic sediments. Such covers, mainly glacial Pleistocene are typica...

Three strong earthquakes ruptured the northwest Thessaly area, Central Greece, on 3, 4 and 12 March 2021. Since area did not rupture by in instrumental period of seismicity, it is great interest to understand seismotectonics source properties these earthquakes. We combined relocated hypocenters, inversions teleseismic P-waveforms InSAR data, moment tensor solutions produce three fault models. T...