MT_ANT2 - Magnetotelluric Measurements Around Neumayer Station III, Antarctica

• Main Authors: Ritter, Oliver, Fromm, Tanja, Weckmann, Ute
• Format: Dataset
• Language: English
• Published: GFZ Data Services 2020
• Subjects: Magnetotelluric; Feasibility Study; Antarctica; Ekström Ice Shelf; Grunehogna craton; EARTH SCIENCE > SOLID EARTH > GEOMAGNETISM > MAGNETIC FIELD > GEOMAGNETIC INDUCTION; In Situ/Laboratory Instruments > Probes; Neumayer; Neumayer Station; Grunehogna; Antarc*; Ice Shelf
• Online Access: https://dx.doi.org/10.5880/gipp-mt.201922.1; https://dataservices.gfz-potsdam.de/panmetaworks/showshort.php?id=escidoc:4979893

Magnetotellurics (MT) is a geophysical deep sounding tool that can help decipher the deep hydrology and geology of Antarctica, in concert with more established and already applied geophysical methods, such as seismology, gravity, and magnetics. Electrical conductivity is an important physical parameter to identify properties of rocks and, perhaps more importantly, constituents within, such as fluids or mineralisation.The unique conditions of Antarctica, which is largely covered with ice cause technical issues, particularly with the electric field recordings, as highly resistive snow and ice at surface of Antarctica hampers contact of the E-field sensors (telluric electrodes) with the ground. The project was a feasibility study to address this principal problem and to test modified MT equipment of the Geophysical Instrument Pool Potsdam (GIPP) in the vicinity of the Neumayer Station III (NMIII) on the Ekström Ice Shelfon. This data publication encompasses a detailed report in .pdf format with a description of the project, information on the experimental setup, data collection, instrumentation used, recording configuration and data quality. The folder structure and content of the data repository are described in detail in Ritter et al. (2019). Time-series data are provided in EMERALD format (Ritter et al., 2015). : The Geophysical Instrument Pool Potsdam (GIPP) provides field instruments for (temporary) seismological studies (both controlled source and earthquake seismology) and for magnetotelluric (electromagnetic) experiments. The GIPP is operated by the GFZ German Research Centre for Geosciences. The instrument facility is open for academic use. Instrument applications are evaluated and ranked by an external steering board. See Haberland and Ritter (2016) and https://www.gfz-potsdam.de/gipp for more information.