Student-reports

Published Aug. 9, 2023 2:20 PM

Lea Belosa is a 3rd-year Phd candidate at CEED (The Centre for Earth Evolution and Dynamics), now PHAB (Centre for Planetary Habitability) at the University of Oslo (UiO). She studies complex dynamic settings near a volcanic edifice in NE Atlantic and their interplay. This winter/spring, she got to experience summer/fall on the other side of the globe – Australia.

Published Apr. 17, 2023 11:21 AM

Linda Haaland, is a third-year PhD student at NTNU in Trondheim. She study the interplay between tectonics and geomorphology, and have a background in structural geology and tectonics. This summer, after a long winter and spring of planning, she finally made it to Svalbard to complete the dataset necessary for her PhD project. Read her story and see great photos from the scenery at Svalbard in her recent blog report as DEEP-student. 

Published Jan. 27, 2022 4:48 PM

This summer, after a year of planning and cancelling travel due to the pandemic, I finally got to visit Svalbard in search of the most valuable thing a young researcher can get: data.

Published Feb. 5, 2020 9:23 AM

My opportunity to collaborate with the magma research group at the Earth Science research laboratory of Orleans to perform high-temperature high-pressure experiments using an internally-heated pressure vessel.

Published Jan. 25, 2019 11:06 AM

Necking to distal domain transition in the offshore mid-Norway; an analogue for the complex western South Atlantic passive margin. Exploration and development Latin-American symposium, Bogotá, Colombia

Published Oct. 31, 2017 10:59 AM

I am a first year PhD candidate in geodynamics at the University of Bergen. My project evaluates the concept of metamorphic core complexes for the Devonian collapse of the Caledonian Orogen in SW Norway. In metamorphic core complexes, deep crustal rocks (the so-called “metamorphic core”) are being exhumed below extensional shear zones and exhibit a close interaction between deep and shallow crustal processes. Furthermore, such structures can significantly influence subsequent tectonic phases like the Mesozoic North Sea rift in case of SW Norway.

Published May 8, 2017 4:19 PM

I was invited to attend a research trip organised by a group of Australian ore geology experts to the Broken Hill district, Australia. Broken Hill, discovered in 1884, is the largest Pb-Zn-Ag deposit in the world, and 250 million tonnes of high-grade ore has been produced from the 8 km long boomerang shaped ore body. The deposit is hosted by a sequence of metavolcanic to metasedimentary rocks in the Palaeoproterozoic Curnamona province, formed at about 1685 Ma.

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