Dana Silerova

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Long-lived (180 Myr) ductile flow within the Great Slave Lake shear zone Dana Silerova The Great Slave Lake shear zone (GSLsz) is a type example for deeply eroded continental transform boundaries located in the Northwest Territories, Canada. Formed during the …

Dana Silerova Read More »

Jokhongir Khayrullaev

Exploring subsurface by means of a generalization of Dix’ classic time-to-depth mapping method Jokhongir Khayrullaev Primary goal of ongoing the research work is to develop new tools in compressional waves (P-waves) domain for exploring the subsurface by means of a …

Jokhongir Khayrullaev Read More »

Tony Doré

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Continental-scale strike-slip faults and their influence on Atlantic and Arctic break-up Tony Doré (EGI,Uni of Utah) Abstract: An idea that has wide currency in plate tectonics is that extending continental margins will undergo gradual stretching, including the exhumation of continental …

Tony Doré Read More »

EGU practice talks

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Thomas Theunissen Oblique continental rifting. Insights from 3-D forward coupled geodynamic-surface process modelling and application to the Equatorial passive margins formation   Leonardo Pichel Geodynamic modelling of salt-bearing rifted margins: from minibasin- to margin-scale salt tectonics across different margin types …

EGU practice talks Read More »

Mike Hudec

Interaction between salt and mobile shale in the East Breaks foldbelt, Northwestern Gulf of Mexico Mike Hudec Bio: The main focus of my research is salt tectonics, particularly kinematic models for evolution and growth of salt structures. This interest began …

Mike Hudec Read More »

Helene Meling Stemland

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Passive seismic monitoring of an arctic glacier Helene Meling Stemland Widespread glacier loss is observed in the Arctic region, partly caused by rising surface temperatures. Calving, which is the mechanical break-off of ice at the glacier terminus, is important to …

Helene Meling Stemland Read More »

Matteo Ravasi

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Seeing through the CO2 plume: joint-inversion segmentation of the Sleipner 4D dataset Matteo Ravasi 4D seismic inversion is the leading method to monitor fluid flow dynamics in the subsurface, with applications ranging from enhanced oil recovery to subsurface CO2 storage. …

Matteo Ravasi Read More »

Martin Muravchik

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

AUV High-Resolution Bathymetry Of Axial-Transverse Drainage Interaction In The Structurally Controlled Subaqueous Channels In The Gulf Of Corinth, Corinth Rift, Greece Martin Muravchik New high-resolution (submeter) bathymetric data, acquired using an AUV Hugin 1000, from the Gulf of Corinth, Greece …

Martin Muravchik Read More »

Tena Belinić Topić

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

Exploring the lithospheric structure beneath the Dinarides using seismograms of teleseismic earthquakes  Tena Belinić Topić The Dinarides are a mountain range located in southeastern Europe with significant tectonic activity and complicated geologic history shaped by the collision of the Adriatic …

Tena Belinić Topić Read More »

David Whipp

Kontinentalsokkelen (2G16e) Realfagbygget, Allégaten 41, Bergen, Norway

David Whipp Can it be all so simple? Challenges and considerations applying thermochronology to understand crustal dynamics Speaker is David Whipp Professor, Department of Geosciences and Geography Institute of Seismology Helsinki Institute of Sustainability Science (HELSUS) Supervisor for doctoral programme, …

David Whipp Read More »