Robert Reinecke
2024-09-26 12:15 - 13:00 (Europe/Oslo) | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
How to use an impossible map – uncertainties in modeling the global water cycle
Robert Reinecke (Guest at the Department invited by Elco Luijendijk)
Global water models allow us to explore the terrestrial water cycle in an earth-sized digital laboratory to guide science and policy. These models simulate increasingly complex representations of different compartments, such as groundwater, and complex processes, such as seawater intrusion. They are coupled with other models, bringing us closer to a digital twin of Earth and enabling us to carry out complex impact assessments of the far future. At the same time, bias-corrected seasonal forecasts allow us to use these models as a window into the near future. However, global water models remain highly uncertain and evaluating them remains challenging. Multiple pathways can be taken to reduce these uncertainties by collecting available knowledge in new ways and analyzing this data with new approaches. In this talk, I will outline new strategies for assessing these complex models differently and rigorously and develop more sustainable research software for a robust science.

Océane Foix
2024-10-02 00:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
From local travel time tomography to seismotectonic models.
Océane Foix, ISTerre, UGA, Grenoble, France
From the creation of seismic databases to seismic travel time tomography and seismic hazard, my aim is to present my career as a young researcher over the last 5 years. I have been able to study different tectonic systems and contexts, such as the deformation of the Vanuatu central subduction forearc (tomography), the seismo-volcanic crisis of Mayotte (tomography) and finally the seismic hazard of the Lesser Antilles subduction (seismotectonic model). At present, I’m using my knowledge to assess the effect of mantle wedge seismicity in the Lesser Antilles on seismic hazard calculations.

Lucie Alain and Agustin Scotti
2024-10-16 00:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Field stories from Eastern Greenland

Presenters Lucie Alain, Agustin Scotti
The DeepReservoir project aims to investigate the distribution and geometry of chlorite-coated intervals in the Early Jurassic Tilje Formation and its analogue in Eastern Greenland. This summer the DeepReservoir team had the chance to go to Jameson Land in eastern Greenland to collect data for the project. Come along to get a chance to see the amazing landscape of Liverpool Land and to hear about what animal were worst than polar bears.

Marianna Anichini
2024-10-30 12:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Marianna Anichini
Reaching the end of the world and back. Stories from the HiAOOS expedition in the high Arctic
Being at sea has always been my dream. Sailing in a sea covered by ice has been an experience that went beyond my expectations. Explorations of this kind are rare and can represent a milestone from personal and scientific perspectives. With some pictures, I will tell you the story of this expedition, how we can study seismic events in such remote places and try to describe emotions that fuel the passion for the work we do.

Maren Kjos Karlsen
2024-11-06 00:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
A NEW NATIONAL SEISMIC HAZARD ASSESSMENT FOR NORWAY
Maren Kjos Karlsen
Do we have earthquakes and do we need to care? An overview of present and past earthquakes and related shaking, our aims to forecast future activity and shaking, and what our preliminary results are telling us.

Isabelle Lecomte
2024-11-13 12:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Ground-Penetrating Radar: fun with rapid underground imaging!
Isabelle Lecomte
Ground-Penetrating Radar (GPR) is probably the most popular geophysical tool for shallow-underground imaging. Its range of application is wide and movies even portray it, e.g., in crime- (forensics) or archaeology-related films. Though using EM-waves instead of elastic ones, GPR’s acquisition principles and processing/imaging have much similarities with seismic. But EM-waves are extremely fast and getting images with GPR is thus a dream compared to seismic! This gives us a tool which is very handy for geophysical education in wave methods and signal processing, while being applicable to various ground-imaging issues as will be illustrated.

Mathilde Bøttger Sørensen
2024-11-20 00:15 - 13:00
EPOS-Norway – Research Infrastructure for Geohazards (EPOS-NG)
Mathilde Bøttger Sørensen
The EPOS-Norway – Research Infrastructure for Geohazards (EPOS-NG) will be established, starting from early 2025, with funding from the Research Council of Norway’s Infrastructure program. EPOS-NG aims to be the go-to infrastructure for research on geohazards in Norway (i.e., landslides, tsunamis, earthquakes, and cryospheric hazards). Complementary to EPOS ERIC and building on research infrastructure developed during EPOS-Norway (EPOS-N) phase 1, EPOS-NG will establish new pools of instruments that are easily accessible to all geoscientists in Norway. We will develop an enhanced and extended state-of-the-art data portal to provide nationwide access to a range of geoscience data as well as computational and visualisation services. The EPOS-NG instrument pools include rapid-deployable seismometers, ocean bottom seismographs, Distributed Acoustic Sensing and Distributed Temperature and Strain Sensing instrumentation, Transient Electromagnetic measurement capacity, piezometers, self-potential sensors and ground-based interferometric radar systems. The new instruments will facilitate research on a wide range of processes including seismicity, slope stability and landslides, groundwater and soil conditions, permafrost and cryospheric processes. Combined with new services for tsunami hazard assessment, as well as novel datasets on InSAR displacement trends and historical and palaeoseismological events, new links can be established through comprehensive, multidisciplinary studies. Effective data integration and visualisation will be achieved via the EPOS-N portal, which was developed in EPOS-N phase 1 and will be substantially enhanced in close dialogue with the users in EPOS-NG. The portal combines data from distributed monitoring networks, innovative services for advanced data analysis and national databases within geosciences into a single national e-infrastructure, following FAIR principles. EPOS-NG thus represents a unifying nationwide research infrastructure, including all the relevant physical infrastructures and providing a national hub for solid Earth science data and services. In this presentation, I will present the plans for EPOS-NG and describe how the community can be involved in and benefit from the activities.

Sebastian Wolf
2024-12-04 00:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
How to invert extensional basins – modelling the influence of pre-collisional extension on 3D mountain belt architecture
Sebastian Wolf
The geological record shows that many orogens, like the Andes, Pyrenees, Atlas, and Greater Caucasus form to a large degree by inversion of pre-collisional extensional basins that are typically offset and show different degrees of basin linkage. However, the 3D dynamics of inverting offset extensional basins and their importance for mountain building remain poorly understood. To bridge that knowledge gap, we use 3D state-of-the-art geodynamic models coupled to a fluvial surface processes model to investigate the dynamics of extensional-basin inversion during continent-continent collision. We find that a) basins link during the extensional stage if basin off-set is not too large; b) inversion of off-set rift basins naturally tends to create opposite polarity subduction, which reverts the plan-view structure of the mountain belt; c) same-polarity subduction requires further weaknesses, but preserves the structure of the extensional basins in the mountain belt. The distribution and orientation of topography and fluvial valleys tracks the deep-structure and can be used as indicators. Based on these model characteristcs and backed by a force-balance analysis, we compare the model results to the Pyrenees, Atlas, and Greater Caucasus.

Albina Gilmullina
2024-12-11 12:00 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Cretaceous source to sink system on the Norwegian Continental Shelf
Albina Gilmullina
The several kilometers thick succession of Cretaceous strata on the Norwegian Continental Shelf bears witness to a period characterised by contemporaneous hinterland uplift, basin subsidence and high sedimentation rates. The northern part of the NCS – informally referred to as the Greater Barents Sea Basin (GBSB) – represented an epicontinental sea dominated by mud-dominated clinoforms exhibiting a wide range of progradational directions. Multiple source areas have thus been suggested based on paleocurrent measurements onshore Svalbard, seismic mapping, petrological analyses, as well as limited provenance data. Although the Lower Cretaceous succession has received considerable attention, Upper Cretaceous strata, which is severely eroded across much of the area, is under-explored. Therefore, volumetric calculations and an in-depth understanding of provenance variations for the whole Cretaceous succession of the GBSB are currently lacking.
In this study, we use >3500 2D seismic lines over the area of 1.500.000 km2 to map Cretaceous sequences from the Eastern and Western Barents Sea and calculate sediment input rates (megatons/year) for eight different seismic units spanning from the Valanginian to the Campanian. We provide new detrital zircon dates from the Lower Cretaceous succession onshore Svalbard. Collectively, this provides insights into sediment volumes, provenance and sediment supply variations during the Cretaceous in the GBSB.

Edoseghe Edwin Osagiede
2025-01-15 00:15 - 13:00
CO2 storage in unconventional geological units – preliminary data from fieldwork in Iceland along the Husavik-Tjornes Peninsula
Edoseghe Edwin Osagiede

Kurt Wogau
2025-01-22 00:15 - 13:00
The Little Karoo: The semi-arid paleolandscape inhabited by the first modern humans”.
Kurt Wogau
In southern Africa, past climate and landscape features could play a relevant role in the evolution of anatomically modern humans and their dispersal through the continental interior during the Marine Isotope Stage (MIS) 5(-71-130 ka) and MIS 4 (~71-57 ka). Our project will shed light on the terrestrial landscape inhabited by Middle Stone Age hunter-gatherers. To reach this aim, we will conduct our research in the Little Karoo, South Africa to assess the paleo-landscape evolution during diverse climatic events (e.g., MIS 5 and MIS 4). The sedimentary record of diverse natural archives such as pan systems, dune fields, and floodplains will be studied.

Thomas Theunissen
2025-01-29 12:15 - 13:00
Interaction of tectonics and surface process during oblique rifted margin formation. Insights from 3-D forward coupled geodynamic-surface process modelling.
Thomas Theunissen
The magma-poor passive rifted conjugate margins in the Southern Equatorial Atlantic, North Atlantic/Arctic oceans, and Northern Mozambique Channel display en-echelon extensional segments separated by long transform faults (>300 km), influenced by inherited weaknesses. Using advanced 3-D forward geodynamic modeling coupled with surface processes, we investigate the formation of oblique rifts and passive margins. Our focus is on pre-existing weaknesses parallel to the extension direction, exploring the system’s sensitivity to various erodibility factors. Key findings include: (1) erodibility within a low to moderate range has limited influence on the morpho-structural evolution of the oblique continental rift, (2) pure-strike slip faults reactivating transform weaknesses result in reduced topography, (3) major catchments sink in the inner corner at the tip of each extensional segments, and (4) hinterland drainage network capture along extensional segments is absent, controlled by isostatic rebound during rift flank drainage divide migration. This study enhances our understanding of the complex nterplay between inherited weaknesses, erodibility, and the evolving morphology of oblique rifted margins.

Kirabo E. Mugwanya
2025-02-12 00:15 - 13:00
Tectonic and Sedimentary Evolution of the Triassic Deposits on the Horda Platform, Norwegian Continental Shelf
Kirabo E. Mugwanya
The Horda platform on the Norwegian Continental Shelf hosts major petroleum fields like Troll and CO₂ storage sites such as the Northern Lights. However, the Triassic deposits remain underexplored for reasons of low data coverage and quality. Using seismic and wireline data, this study illustrates the evolution of major faults and its role on the basin’s sedimentology. The Horda platform hosts over 5 km of rapidly deposited (c. 50 Ma) alluvial sediments, formed under a shifting arid to humid climate, with varying tectonic activity and potential rapid orogenic denudation. Tectono-stratigraphic reconstructions of the sub-basins are presented to illustrate the control of tectonic evolution on the spatial and temporal facies distribution and the stratigraphic architecture. A case of a mega-scale mass movement (?) driven by fault detachment and evidence of early Triassic erosional uniformity are additionally illustrated.

Robert Reinecke
2025-02-19 00:15 - 13:00
How to use an impossible map – uncertainties in modeling the global water cycle
Robert Reinecke
Global water models allow us to explore the terrestrial water cycle in an earth-sized digital laboratory to guide science and policy. These models simulate increasingly complex representations of different compartments, such as groundwater, and complex processes, such as seawater intrusion. They are coupled with other models, bringing us closer to a digital twin of Earth and enabling us to carry out complex impact assessments of the far future. At the same time, bias-corrected seasonal forecasts allow us to use these models as a window into the near future. However, global water models remain highly uncertain and evaluating them remains challenging. Multiple pathways can be taken to reduce these uncertainties by collecting available knowledge in new ways and analyzing this data with new approaches. In this talk, I will outline new strategies for assessing these complex models differently and rigorously and develop more sustainable research software for a robust science.

Giulio Di Toro
2025-03-05 12:15 - 13:00
Seismic cycle in the presence of hot and pressurized fluids
Giulio Di Toro
Geophysical evidences and the investigation of exposed faults exhumed from upper crustal depths indicate that earthquakes nucleate and propagate often in the presence of fluids at “hydrothermal conditions” typical of geothermal systems (temperature and fluid pressure: 150°C < T 25 MPa). However, also because of technical difficulties in performing rock deformation experiments under such extreme conditions, the evolution of frictional properties of fault materials that contribute to the seismic or aseismic behavior of the fault/fracture network is poorly known.
Here, motivated by the study of fault zones exhumed from 4-8 km depth, we will discuss the results (mechanical data, microstructural-mineralogical-geochemical analysis, etc.) of experiments performed with new devices which combine rotary shear machines and hydrothermal vessels. These experimental devices can reproduce hydrothermal conditions in the laboratory by imposing on simulated faults aseismic (nm/s) to seismic (m/s) slip rates and slip distances up to several meters in the presence of hot (up to 500°C) and pressurized (up to 70 MPa) fluids. Based on the results obtained with these devices, we will discuss fluid-rock interaction, pressure and temperature of the fluid and stress loading in earthquake nucleation and healing of faults of the upper crust (Bolfin fault zone, Atacama Fault System, Chile; Krafla geothermal system, Iceland).
The main objective of this multidisciplinary scientific approach is to reveal (i) the main factors responsible for the seismic and aseismic behavior of natural faults, (ii) how fractures and faults “heal” during the seismic cycle, and (iii) the deformation mechanisms that operate under hydrothermal conditions. These results could indicate new methods for a safer exploitation of deep geothermal reservoirs.

Eivind Olavson Straume
2025-03-19 12:15 - 13:00
The influence of paleogeography on Cenozoic ocean circulation and climate
Eivind Olavson Straume
Paleogeography, influenced by plate tectonics, mantle convection, volcanism, erosion, and sedimentation, cause large-scale ocean circulation and climate changes on geological timescales. Some of the most important paleogeographic changes are linked to opening and closing of key oceanic gateways connecting the world’s major oceanic basins. During the Cenozoic (66 – 0 Ma), several gateways opened and closed (e.g. the Atlantic – Arctic gateways, Tethys Seaway, West Siberian Seaway, and the Southern Ocean gateways), which played an important role in the complex transition from greenhouse to icehouse climate during this time interval. This presentation will mainly focus on the role of paleogeography of oceanic gateways and their impact on ocean circulation, climate and biogeography. I will present a new global Digital Elevation Model (DEM) for the Cenozoic time, with updated regional reconstructions for the closure of the Tethys Seaway, West Siberian Seaway, and opening of the Atlantic – Arctic gateways. These regions were influenced by deep earth processes such as mantle convection and played a key role in shaping the modern global ocean circulation. I will present Earth system model experiments showing the simulated impact on ocean circulation and climate. Ultimately linking deep and solid earth changes, to changes in ocean circulation, climate, and biogeographic dispersals.
snapshot from an animation showing paleogeography and reconstructed mantle densities for the Eocene-Oligocene transition (34 Ma).
Eivind Olavson Straume – Biography (Using ChatGPT)
Dr. Eivind Olavson Straume is a Norwegian geoscientist specializing in paleoclimate, plate tectonics, and mantle dynamics. He is currently a postdoctoral researcher at NORCE Norwegian Research Centre, where he investigates the interactions between tectonics, oceanic gateways, and climate evolution over geological time scales.
Straume earned his Ph.D. from the University of Oslo (UiO) in 2020, defending his dissertation Paleoclimate in the Cenozoic Time: Quantifying the Role of North Atlantic Plate Tectonics and Mantle Processes. His research focuses on reconstructing past oceanic and atmospheric conditions using numerical modeling and geological data, particularly emphasizing the impact of plate tectonics on ocean circulation and climate variability.
He has contributed significantly to global paleobathymetric reconstructions, developing methodologies for estimating sediment thickness and modeling oceanic gateways’ influence on climate transitions. His work has been published in high-impact journals such as Nature Reviews Earth & Environment, Earth and Planetary Science Letters, and Proceedings of the National Academy of Sciences (PNAS).
Beyond his academic research, Straume is an advocate for open science and data visualization. He co-founded s-Ink.org, an initiative aimed at making geoscience graphics more accessible. He has also participated in numerous scientific outreach events, sharing insights on plate tectonics, climate change, and Earth’s dynamic systems.
Currently based in Bergen, Norway, Dr. Straume continues his research at NORCE, collaborating with leading geoscientists to refine models of Earth’s climatic and geological evolution.
Main Collaborators and Ph.D. Supervisors of Eivind Olavson Straume
Ph.D. Supervisors (University of Oslo, CEED/Department of Geosciences)
Prof. Carmen Gaina (CEED, UiO) – Expert in plate tectonics and geodynamics.
Prof. Joseph Henry Lacasce (Department of Geosciences, UiO) – Specialist in ocean dynamics and climate modeling.
Prof. Kerim Hestnes Nisancioglu (Bjerknes Centre for Climate Research, UiB) – Focuses on paleoclimate and ocean circulation.
Main Collaborators
Throughout his career, Dr. Straume has worked closely with several leading geoscientists, including:
Grace Shephard (UiO, CEED) – Collaborated on geodynamic and tectonic reconstructions.
Fabio Crameri (UiO, CEED) – Worked on scientific visualization and geoscience graphics.
Sergei Medvedev (UiO, CEED) – Contributed to paleobathymetry and geodynamic modeling.
Aleksi Nummelin (UiB) – Collaborated on climate modeling and ocean dynamics.
Bernhard Steinberger (GFZ Potsdam) – Worked on mantle convection and dynamic topography.
Claudio Faccenna (Roma Tre University) – Studied the influence of mantle dynamics on paleogeography.
Zhongshi Zhang (NORCE, UiB) – Focused on paleoclimate simulations.
Carmen Gaina (UiO) – Ongoing collaboration on Arctic and Atlantic paleogeography.
Agatha M. de Boer (Stockholm University) – Worked on ocean circulation and climate reconstruction.
Stephanie Werner (UiO, CEED) – Collaborated on tectonics and mantle dynamics.
His work also involves contributions from various institutions, including the Bjerknes Centre for Climate Research (UiB), NORCE, and international geoscience organizations.

Christopher Campbell Di Paolo
2025-03-26 12:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Searching for lacustrine tsunami deposits with the aid of a numerical model
Christopher Campbell Di Paolo
A Mw ca. 5.9 earthquake occurred in 1601 CE in central Switzerland which triggered multiple subaqueous and subaerial landslides in and around Lake Lucerne. One of these subaqueous landslides triggered a tsunami which hit the city of Lucerne. While this tsunami was documented historically, physical evidence remains sparse. Using the numerical modeling software BASEMENT, we simulated the tsunami’s sediment transport. With this model as a guide, we then took 9 sediment cores in areas of interest. We link an event layer which exists in 4 of the 9 cores to the 1601 CE event. The program BASEMENT proved to be effective at simulating lacustrine tsunami sediment transport.

Julien Vadnais
2025-04-09 12:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Deep transfer learning for mapping rare Arctic oil seeps observed from satellites
Julien Vadnais – Department of Earth Science, UiB

Abstract
Natural seepage is a significant contributor to marine oil inputs. Remote and intermittent seeps are difficult to monitor in the field, yet oil slicks can be observed by spaceborne synthetic aperture radar (SAR) because they reduce backscatter, creating potential for automatic mapping. In mapping tasks like segmentation, deep learning models excel, albeit needing large amounts of labeled images. To deal with scarcity of labeled images, transfer learning is an approach commonly used in computer vision, though still underutilized in remote sensing.
Different Sentinel-1 acquisition modes, in the Arctic compared to elsewhere, complicate direct model transfer for oil slick mapping. Here, we present a use-case where transfer learning enhances the segmentation of natural oil slicks, most notably in challenging and noisy images. Our method proves efficient even with limited training images, offering new prospects for studying poorly understood or yet undiscovered hydrocarbon seeps.

Chawnghlut Lallawmawma and Mudit Srivastava
2025-04-23 12:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Title TBD
Chawnghlut Lallawmawma
Mudit Srivastava
Abstract
TBD

Xiaoyue Wang
2025-04-30 00:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Title TBD
Xiaoyue Wang

Abstract
TBD

Bayani Cardenas
2025-05-07 00:15 - 13:00 | Auditorium 5, 3rd floor, Realfabyyget, 41 Allégaten, Bergen, 5007, Norway
Ridge to reef volcanic hydrogeology: submarine groundwater in the world’s most biodiverse coasts
Bayani Cardenas – Jackson School of Geosciences, The University of Texas at Austin

Abstract
Water flows from land to the ocean not only through rivers and estuaries but also below-ground through coastal and submarine aquifers. While the global fresh submarine groundwater discharge (SGD) is less than nutrient inputs are 25% of riverine inputs. This land-ocean connectivity is important for sensitive ecosystems such as coral reefs if the groundwater we present the interesting but in the Philippines which has been coral reefs provide for local communities. We studied coastal and submarine thermal springs associated with high fluxes of acidic waters and carbon dioxide, some of which are within or close to thriving coral reefs. The SGD fluxes are amongst the largest in the world and the SGD carbon dioxide fluxes overwhelm coastal carbon budgets. The presentation delivers explanations for the high SGD, discussing the mechanics and different sources and pathways of water, by bringing together multiple lines of evidence from different methods including deep diving, drones, novel sensors, geochemical tracers, thermal remote sensing, and modeling.

Martin Muravchik
2025-05-14 12:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
TITLE TBD
Martin Muravchik – Department of Earth Science, UiB

Abstract
TBD

Simon Bufféral
2025-05-21 00:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Title TBD
Simon Bufféral – ENS, Paris

Abstract
TBD

Ingra Malucelli Barbosa
2025-05-28 00:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Title TBD
Ingra Malucelli Barbosa – Department of Earth Science, UiB

Abstract
TBD

Francina Saiz Garcia
2025-06-04 00:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Title TBD
Francina Saiz Garcia – Department of Earth Science, UiB

Abstract
TBD

Grant Ferguson
2025-06-11 00:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Title TBD
Grant Ferguson

Abstract
TBD

Kirabo E. Mugwanya
2025-06-18 00:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
Title TBD
Kirabo E. Mugwanya – Department of Earth Science, UiB

Abstract
TBD

Leonardo Muniz Pichel
2026-02-11 12:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway

Sebastian Wolf
2026-03-04 12:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway

Severine Russo
2026-03-11 12:15 - 13:00 | Kontinentalsokkelen (2G16e), Realfagbygget, Allégaten 41, Bergen, 5007, Norway
