UKGEOS Glasgow post-drill bedrock model

Kearsey, Tim | Burkin, Joel

2021

The UK Geoenergy Observatories (UKGEOS) Glasgow bedrock model outputs, created by the British Geological Survey, provide a semi-regional overview of the depth and extent of bedrock lithostratigraphic units, coals and faults. The model allows users to visualise the likely subsurface sequence...

UKGEOS Glasgow post-drill superficial deposits model

Arkley, Sarah | Callaghan, Eileen

2021

The UK Geoenergy Observatories (UKGEOS) Glasgow superficial deposits GSI3D model outputs, created by the British Geological Survey, provide a semi-regional overview of the depth, thickness and extent of glacial and post-glacial lithostratigraphic units above rockhead. The model allows users...

UKGEOS Cheshire - TH0424 Final Borehole Information Pack

UKGEOS Cheshire Project Team

2023

The final borehole information pack from the TH0424 Ground Investigation Borehole drilled as part of the UK Geoenergy Observatories (UKGEOS) Cheshire facility. TH0424 was drilled to TD of 101 m between the 08-Nov-2021 and 30 Nov-2021. Drill core was collected from 2 m – 101 m with 100 mm...

UKGEOS Cheshire - BHA-101 Initial Borehole Information Pack

Hetherington, David | Damaschke, Magret | Thompson, Joanna | Hough, Edward | Kingdon, Andrew | Spence, Mike | Cripps, Catherine | Elsome, Jack | Burgess, Daniel | Fellgett, Mark

2022

This data pack contains information from geotechnical and contaminated land investigations carried out at potential sites for the development of the UK Geoenergy Observatory in Cheshire. Following these investigations, a decision was made to move the proposed observatory to Thornton Science...

UKGEOS Cheshire - TH0424 Initial Borehole Information Pack

Hetherington, David | Fellgett, Mark | Damaschke, Magret | Kingdon, Andy | Elsome, Jack

2022

The initial borehole information pack from the TH0424 Ground Investigation Borehole drilled as part of the UK Geoenergy Observatories (UKGEOS) Cheshire facility. TH0424 was drilled to TD of 101 m between the 08-Nov-2021 and 30-Nov-2021. Drill core was collected from 2 m – 101 mm with 100 mm...

Dataset of the 6G seismic network at Los Humeros, 2017-2018

Toledo, Tania | Gaucher, Emmanuel | Metz, Malte | Calò, Marco | Figueroa, Angel | Angulo, Joel | Jousset, Philippe | Kieling, Katrin | Saenger, Erik

2019

Extensive passive seismic monitoring was carried out between September 2017 and September 2018 over the Los Humeros geothermal field in Mexico. This experiment, in addition to several geophysical, geological, and geochemical surveys was conducted in the framework of the European H2020 and...

Data of the temporary seismic WILAS network

Dias, N.A. | Silveira, G. | Haberland, C.

2010

The lithosphere of Iberia has been formed through a number of processes of continental collision and extension. In Lower Paleozoic, the collision of three tectonics blocks produced the Variscan Orogeny, the main event of formation of the Iberian lithosphere. The subsequent Mesozoic rifting...

Seismic sensing of hydraulic and sediment transport patterns below frozen subarctic river

Dietze, Michael | Polvi, Lina

2019

Our understanding of the effects of ice on channel morphodynamics and bedload transport in northern rivers, frozen for several months, are hindered by the difficulties of ‘seeing’ through the ice. We use continuous seismic records of a small network at the Sävar River in northern Sweden to...

Landscape Response to the Mw7.9 Gorkha Earthquake

Andermann, Christoff | Sens-Schönfelder, Christoph | Turowski, Jens

2015

Strong earthquakes cause transient perturbations of the near Earth’s surface system. These include the widespread landsliding and subsequent mass movement and the loading of rivers with sediments. In addition, rock mass is shattered during the event, forming cracks that affect rock strength and...

ISMENET - ISMEtpasa seismic NETwork

Becker, Dirk | Chen, Xiang | Martinez-Garzon, Patricia

2023

15 station seismological network spanning the North Anatolian Fault Zone (NAFZ) toward the east of Ismetpasa to detect possible microseismicity and slow slip events in the creeping section of the NAFZ. The network consists of 10 three component 4.5 Hz geophone sensors in combination with...