GP31A-3667:
A Novel Approach to Asynchronous MVP Data Interpretation Based on Elliptical-Vectors

Wednesday, 17 December 2014
Mikhail Kruglyakov1, Igor Trofimov2, Sergey Korotaev2, Vitaly Shneyer2, Irina Popova2, Darya Orekhova3, Yury Scshors4 and Michael Semenovich Zhdanov5, (1)Lomonosov Moscow State University, Moscow, Russia, (2)Schmidt Institute of Physics of the Earth RAS, Moscow, Russia, (3)NIC "Kurchatov Institute", Moscow, Russia, (4)NIC, Moscow, Russia, (5)University of Utah, Salt Lake City, UT, United States
Abstract:
We suggest a novel approach to asynchronous magnetic-variation profiling (MVP) data interpretation.

Standard method in MVP is based on the interpretation of the coefficients of linear relation between vertical and horizontal components of the measured magnetic field.

From mathematical point of view this pair of linear coefficients is not a vector which leads to significant difficulties in asynchronous data interpretation. Our approach allows us to actually treat such a pair of complex numbers as a special vector called an ellipse-vector (EV). By choosing the particular definitions of complex length and direction, the basic relation of MVP can be considered as the dot product. This considerably simplifies the interpretation of asynchronous data.

The EV is described by four real numbers: the values of major and minor semiaxes, the angular direction of the major semiaxis and the phase. The notation choice is motivated by historical reasons.

It is important that different EV's components have different sensitivity with respect to the field sources and the local heterogeneities. Namely, the value of major semiaxis and the angular direction are mostly determined by the field source and the normal cross-section. On the other hand, the value of minor semiaxis and the phase are responsive to local heterogeneities.

Since the EV is the general form of complex vector, the traditional Schmucker vectors can be explicitly expressed through its components.

The proposed approach was successfully applied to interpretation the results of asynchronous measurements that had been obtained in the Arctic Ocean at the drift stations “North Pole” in 1962-1976.