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A combined TEM-MT survey was carried out in the Montelago geothermal prospect, situated on Mindoro Island, the Philippines, with the aim to obtain the dimensions and depth of the geothermal reservoir as well as to formulate the prospects' conceptual model. The acquired MT data are static shift corrected using the TEM measurements. Two different 3D...
In June 2013 a 51-station magnetotelluric (MT) survey was carried out to investigate the geothermal prospectivity of an area located in the Aegean Coastal Belt in northwestern Turkey. The metamorphic unit that is generally inferred to host the geothermal reservoir is of Paleozoic age and contains a granitic batholith which intruded the unit during...
In June and July 2013 a 51 station combined AMT and MT survey was carried out for the exploration of a geothermal prospect in Western Turkey. The data was acquired using both Phoenix MTU-A and Metronix ADU-07e data loggers. The two instrument types were distributed evenly over the number of stations, but unevenly over the exploration area with Metr...
A Multi-Energy Concept comprising both low enthalpy geothermal energy and shallow high temperature heat storage is designed to sustainably heat a greenhouse area in the Netherlands. The geothermal system will produce heat year-round to a district heating
Pursuit and use of geothermal energy in the Netherlands is developing steadily. However, in order to make sound decisions, investors and insurers are requesting the probability of success of each planned geothermal project. A methodological appraisal system was developed in order to achieve a meaningful probability of success of the expected flow r...
In 2007 a geothermal project was realized for a tomato grower in Bleiswijk, The Netherlands. This project was realized in a cretaceous sandstone reservoir at a depth of approximately 1,700 m. Since then, numerous other greenhouse owners became interested in this energy source. However, the subsurface area required for the heating of a greenhouse is...
Investigate the feasibility of the MT and CSMT method for geothermal exploration in the Netherlands. We will try to answer question as: - Will we see a sandstone reservoir at 2 km depth? - What will be the influence of EM cultural noise? - Will we be able to estimate porosity and permeability of the reservoir? - Will we be able to see faults?