This week, Angela has been busy delivering core gifts around the Aberdeen area. It's for a project we worked on a lot, as it's been one of the biggest ones we've had recently. Now that most of them have left HQ, there's finally some room to move about again!
05.09.2025 08:31 β π 1 π 0 π¬ 0 π 0
A recent core donation brought in some red beds that we don't often see in North Sea wells - the Devonian. The photos show parts of core number 2 from 37/12-1. Most of the interval consists of rather broken-up and dull bits of claystone, but as is often the case, there is the odd nice bit!
15.08.2025 11:45 β π 1 π 0 π¬ 0 π 0
Bits of core used for gifts
What's better than receiving a bit of core after delivering a talk?
That's what the organisers of the PGK monthly technical talks thought over the past few years.
We recently supplied them with a new batch of gifts that will hopefully land on desks and will be looked at for years to come!
01.08.2025 10:43 β π 1 π 0 π¬ 0 π 0
YouTube video by GEO EXPRO
Coring Step by Step - GEO EXPRO & Reservoir Group
We talk about core all the time, but what does it take to get it out of the ground? In a project with GEO EXPRO, we visited Reservoir Group in Aberdeen and talked to Coring Manager Europe Steve Rait, who walked us through the main elements of a coring assembly.
www.youtube.com/watch?v=ad_X...
04.07.2025 08:40 β π 0 π 0 π¬ 0 π 0
An oil spill in a core ππ½
We have seen a fair bit of core, but this little oil spill was new for us. It sits in a thin and fine-grained bit of Buzzard sandstone from exploration well 20/04a-10.
The composite well log does not report shows in this interval above OBM, so what could it be?
26.06.2025 08:32 β π 2 π 0 π¬ 0 π 0
"I have always found it difficult to describe rock properties based only on hand specimens. Working with the cores helped me a lot to understand the sedimentological relationships better and confirmed that my decision to study geology was the right one."
Student at Kiel University in Germany
20.06.2025 09:42 β π 1 π 0 π¬ 0 π 0
As Greenbrae school in Aberdeen has been learning about the Pangea supercontinent, Mariel Reitsma paid a visit yesterday and showed some rocks that were deposited around that time.
Are you interested in a set of cores for your classroom, a visit from us, or a copy of the slides, please let us know.
29.05.2025 12:41 β π 1 π 0 π¬ 0 π 0
In 2020, as the pandemic unfolded, Kirstie and Henk made North Sea Core official.
Now, this handshake is a symbol for Kirstie to move on and focus more on her career.
In the meantime, the rest of the team remains as dedicated as ever.
Kirstie, thank you so much for the work over the years!
22.05.2025 10:27 β π 3 π 0 π¬ 0 π 0
Is this an oil-down-to or an oil-water contact? Lots to see in this beautiful Claymore Sand core that is currently on display at the Devex 2025 Conference in Aberdeen.
Also, this section was accidentally cored as the original target was deeper down.
We are now thankful this happened.. π¬
21.05.2025 10:11 β π 1 π 0 π¬ 0 π 0
This week, we feature a core from the Western Canada foreland basin, showing a Lower Cretaceous section. Based on trace fossil content, Robert MacKeracher, from Mount Royal University, explained that this section was probably deposited in a lacustrine environment rather than shallow marine.
15.05.2025 12:35 β π 7 π 2 π¬ 0 π 0
This core is from the Sirte Basin in Libya. It is an Eocene carbonate and evaporite succession belonging to the Hon Fm, showing an undulated but very sharp transition from anhydrite (gypsum) to carbonate deposition as sea level rose slightly. Isn't it a beauty!
09.05.2025 10:42 β π 2 π 0 π¬ 0 π 0
You don't necessarily need to look at seismic to see nice faults - sometimes a bit of core is enough to observe spectacular examples of structural geology. For example, this bit of Upper Jurassic Claymore Sandstone from well 15/21b-50 near the Telford field in the Moray Firth.
02.05.2025 10:19 β π 33 π 6 π¬ 0 π 1
Thanks to Serica Energy for joining our existing sponsors and further supporting our work!
Sponsors help us in our mission to save, store, and make core available for the next generation of geoscientists.
24.04.2025 11:33 β π 1 π 0 π¬ 0 π 0
Every time our joiner Pat McCabe drops off a selection of newly made frames, it is exciting to see what he's got in his van. This time, it included two Brent frames, showing samples from the Broom, Rannoch, Etive, Ness and Tarbert formations in a row. So nice!
17.04.2025 09:35 β π 3 π 0 π¬ 0 π 0
We asked ourselves at the end of 2023 - has the decline kicked in? Are people tired of seeing core? Actually, the contrary is true: we have shipped to many new places and have diversified in terms of sponsorships and collaborations. Ready for another good year!
10.04.2025 10:23 β π 3 π 1 π¬ 0 π 0
A "normal" sandstone you'd say, but then you check the comp log and it turns out to be a Carboniferous one! This is well 15/19-6 in the Moray Firth, where Carboniferous rocks have hardly been drilled. Also note the fractures at the bottom of the core - maybe one could be drilling induced?
03.04.2025 08:24 β π 0 π 0 π¬ 0 π 0
North Sea Core HQ is getting a upgrade with new racks to help organise all the relinquished core we take in!
20.03.2025 13:21 β π 1 π 0 π¬ 0 π 0
Sometimes itβs hard to say goodbye to the the core products we create! If you fancy a framed piece of stunning Brent core in your home or office, we will reluctantly agree to let these beauties goβ¦ please get in touch at northseacore@gmail.com
13.03.2025 12:26 β π 2 π 1 π¬ 0 π 0
Fantastic to see such a engaged crowd at the GESGB (Geoscience Energy Society of Great Britain) #BEOS2025 Core Workshop, with Henk Kombrink talking through the geological evolution of the North Sea using some of our prized teaching set
06.03.2025 12:17 β π 2 π 0 π¬ 0 π 0
North Sea Core have not started taking in zebras, itβs just the Claymore Sandstone Unit of the Upper Jurassic Kimmeridge Clay Formation! These incredible alternating finely laminated mudstones, fine sandstones and coarser oil stained sandstones are from well 15/21b- 50 #NorthSeaCore #Geology
28.02.2025 13:10 β π 2 π 0 π¬ 0 π 0
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