ALT Figure 1: Flowrate and Allowable drawdown

ALT César Patiño at one of his favourite spots in the Stavanger area; the rock carvings of Fluberget, Revheim. These carvings date back to the Bronze Age (1800-500 BC). Photo: Damir Grskovic.

ALT Seismic line through the Ephesus area, illustrating how the far offset clearly brings out the prospect through its higher amplitudes. Seismic lines kindly provided by Oilco.

ALT An iDrop node

ALT Zoom in on the Urd field area and the Jurassic fault blocks imaged by a GeoStreamer X depth seismic line (Left). At an apex depth of ca. 1,830 m below seabed, high-impedance reflectors can be seen. These are caused by interbedded coals in the Åre Fm (blue arrow). Åre sandstones are proven reservoirs along with overlying Viking Group sandstones. A high degree of fault segmentation is obvious and critical in field development strategies. Note the difference in fault plane visibility, fault plane extent (orange arrows), and reflector termination against the faults (yellow arrows) compared with the single azimuth seismic (Azimuth 34) section in the section on the right.

ALT Bangladesh, a country close to the water line. Photo: Tarek Suman/Unsplash

ALT Marten ter Borgh from EBN presents results of the SCAN seismic acquisition campaign in the Netherlands, which aims to shed more light on the subsurface for geothermal exploration. Photo: Henk Kombrink