In the course of seasonal work of the 70th Russian Antarctic expedition (RAE) in 2024-2025, as part of the field geological and geophysical studies by researchers of Empress Catherine II Saint Petersburg Mining University on the Broknes Peninsula (Larsemann Hills, East Antarctica), areal ground magnetic survey was accomplished at 1:10,000 scale. The study area is characterized by a high exposure degree of Cambrian and Precambrian rocks with localization in certain parts of magnetite-bearing complexes. The work included experimental and methodological research, surveying in two modes (discrete and continuous) with data quality control as well as subsequent processing and initial interpretation of the results. A detailed map of the total magnetic intensity covering an area of 17.5 km 2 and maps of the field transformations – vertical derivative, absolute horizontal gradient, etc., were compiled. Qualitative interpretation allowed identifying morphologically homogeneous zones in the study area characterized by different features of anomalous magnetic field. Results of the studies will be used in future for geological interpretation of anomalies and compilation of the structural tectonic map of the region.
The purpose of this work is to assess the possibilities of using electromagnetic monitoring to study the development of a fracture system generated by hydraulic fracturing (HF) with a specified position of the controlled source. The option with the source (a vertical electric dipole) located in the interval of the oil-bearing formation and ground-based measurements was chosen as the most promising monitoring plan. We have built a geoelectric model equivalent to the system of hydraulic fractures, divided into 11 zones corresponding to HF stages. For the selected model, mathematical simulation was performed by solving the direct problem considering the impact of the steel casing, the presence of which reduced the effect. Despite this fact, no strong distortion of electromagnetic field anomaly was observed above the HF zone. Analysis of the simulation results at different HF stages showed that as new hydraulic fractures appeared and were filled with electrically conductive proppant, the total effect increased. The data on electric field anomaly demonstrated maximum deviation from the background level of more than 2 %. Provided that the studied formation is characterized by sufficient electrical conductivity, its magnetic field also becomes informative.
The article analyses relationships between electrochemical processes in the weathering crust and geochemical fields to estimate the natural electric fields influence on the movement of metal ions in rocks. In situ and laboratory tests data can help to evaluate mass transfer under the influ-ence of electric fields and redistribution of chemical elements in rocks due to electrical phenom-ena. The observed dependences allow confirming the influence of the natural electric field on dif-ferentiation of elements in rocks.
