Phoenix Geophysics
Base and Precious Metals ExplorationOil and Gas ExplorationDiamond ExplorationEnvironmental and Engineering StudiesGeothermal ExplorationReservoir MonitoringGroundwater ExplorationDeep Crustal ResearchEarthquake Prediction Research


Using Automated Array Systems For 4D Time-Lapse Measurements

Many geophysical and geological processes (natural and man-made) cause variation of the earth's physical properties with time. Examples of natural processes include volcanic eruptions, earthquakes, landslides, and hydrological variations.
Man-made processes usually involve movement of fluids in the zone of interest. Such zones include geothermal or hydrocarbon reservoirs; injection wells; underground storage caverns for natural gas or other substances; and producing aquifers.
By monitoring these physical properties over time, the nature of their temporal and volumetric variations can be defined. The resulting knowledge can be used to optimize production processes or to help forecast volcanic eruptions and earthquakes, for example.

The main physical property measured by this system is resistivity. Significant resistivity variations are typical in all the applications mentioned. With Phoenix monitoring equipment and software, the changes can be measured at the surface.
The system features fully automated power supply, data acquisition, and data processing, so manpower requirements are reduced to the minimum. Researchers or operators access key results as graphs, maps, and volumes showing the variation of parameters with time.

To learn more

To learn more about reservoir mapping and monitoring applications of Phoenix MT Instrumentation, please see these newsletter articles:
Hydrocarbon in Brazil Geothermal in Japan
You can also see these PowerPoint slides about Automated Stationary MT Monitoring System

What our Clients say...

Letters of reference from our customers:

deep rapid reconnaissance and detailed follow-up

From near-surface down to any practical drilling depth and beyond, MT allows rapid reconnaissance of areas as large as tens of square kilometers, while detecting conductive zones to 2000 m and deeper.
Closely spaced stations along lines or nets provide data redundancy, high lateral resolution, and a continuous picture of the subsurface resistivity structure.
In a two-pass methodology, station and line spacing are as wide as possible in the first pass to keep cost to a minimum. Once areas of interest have been identified, a second pass with more stations at closer spacing increases resolution. The result is rapid, accurate, and cost-effective identification of conductive mineralized zones.

rapid, cost-effective mapping of conductive zones

Equipment weighs only 30 kg per site, so it's portable by backpack, ATV, snowmobile, or helicopter, from tundra to jungle, in any season. This logistic simplicity reduces cost and increases productivity.
The small footprint and environmentally benign installation make the technique practical almost anywhere.
Flexible site location and offline sensitivity allow meaningful profiles to be constructed without the rigid grid of methods like seismic and IP.
Induction vectors indicate the direction and relative strength of offline conductors and are especially useful where the surface is resistive or frozen (no electrodes required).
MT/AMT sees through the thick conductive clay (impenetrable by airborne or other surface techniques) that covers many prospective areas.
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