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

被引:24
|
作者
Becken, M. [1 ]
Nittinger, C. G. [1 ]
Smirnova, M. [1 ]
Steuer, A. [2 ]
Martin, T. [2 ]
Petersen, H. [2 ]
Meyer, U. [2 ]
Moerbe, W. [3 ]
Yogeshwar, P. [3 ]
Tezkan, B. [3 ]
Matzander, U. [4 ]
Friedrichs, B. [4 ]
Rochlitz, R. [5 ]
Guenther, T. [5 ]
Schiffler, M. [6 ]
Stolz, R. [6 ]
机构
[1] Univ Munster, Inst Geophys, Corrensstr 24, D-48149 Munster, Germany
[2] German Fed Inst Geosci & Nat Resources BGR, Stilleweg 2, D-30655 Hannover, Germany
[3] Univ Cologne, Inst Geophys & Meteorol, Pohligstr 3, D-50969 Cologne, Germany
[4] Metronix Messgerate & Elektron GmbH, Kocherstr 3, D-38120 Braunschweig, Germany
[5] Leibniz Inst Appl Geophys, Stilleweg 2, D-30655 Hannover, Germany
[6] Leibniz Inst Photon Technol, Albert Einstein Str 9, D-07745 Jena, Germany
关键词
AREA;
D O I
10.1190/geo2019-0336.1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
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 4 x 5 km(2) for a single source installation. The system has the potential to be used for focused exploration of deep targets.
引用
收藏
页码:E253 / E267
页数:15
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