DESMEX: A novel system development for semi-airborne electromagnetic exploration

Author:

Becken M.1ORCID,Nittinger C. G.1,Smirnova M.1ORCID,Steuer A.2ORCID,Martin T.2,Petersen H.2,Meyer U.2,Mörbe W.3,Yogeshwar P.3ORCID,Tezkan B.3,Matzander U.4,Friedrichs B.4,Rochlitz R.5ORCID,Günther T.5,Schiffler M.6,Stolz R.6,

Affiliation:

1. University of Münster, Institute of Geophysics, Corrensstrasse 24, Münster D-48149, Germany.(corresponding author); .

2. German Federal Institute for Geosciences and Natural Resources (BGR), Stilleweg 2, Hannover D-30655, Germany..

3. University of Cologne, Institute of Geophysics and Meteorology, Pohligstrasse 3, Köln D-50969, Germany..

4. Metronix Meßgeräte und Elektronik GmbH, Kocherstrasse 3, Braunschweig D-38120, Germany..

5. Leibniz Institute for Applied Geophysics, Stilleweg 2, Hannover D-30655, Germany..

6. Leibniz Institute of Photonic Technology, Albert-Einstein-Strasse 9, Jena D-07745, Germany..

Abstract

There is a clear demand to increase detection depths in the context of raw material exploration programs. Semi-airborne electromagnetic (semi-AEM) methods can address these demands by combining the advantages of powerful transmitters deployed on the ground with efficient helicopter-borne mapping of the magnetic field response in the air. The penetration depth can exceed those of classic airborne EM systems because low frequencies and large transmitter-receiver offsets can be realized in practice. A novel system has been developed that combines high-moment horizontal electric bipole transmitters on the ground with low-noise three-axis induction coil magnetometers, a three-axis fluxgate magnetometer, and a laser gyro inertial measurement unit integrated within a helicopter-towed airborne platform. The attitude data are used to correct the time series for motional noise and subsequently to rotate into an earth-fixed reference frame. In a second processing step, and as opposed to existing semi-AEM systems, we transform the data into the frequency domain and estimate the complex-valued transfer functions between the received magnetic field components and the synchronously recorded injection current by regression analysis. This approach is similar to the procedure used in controlled-source EM. For typical source bipole moments of 20–40 kAm and for rectangular current waveforms with a fundamental frequency of approximately 10 Hz, we can estimate reliable three-component (3C) transfer functions in the frequency range from 10 to 5000 Hz over a measurement area of [Formula: see text] for a single source installation. The system has the potential to be used for focused exploration of deep targets.

Funder

Bundesministerium für Bildung und Forschung

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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