Cretaceous granites-possible source of the Carpathian gravity low

• Magnetotelluric measurements have recently made a significant contribution to the mapping of deep Earth structures in combination with other geophysical methods. • This comprehensive method of studying the Earth's crust allows for the determination of the composition of this hitherto little-explored part of the Western Carpathians with increasing certainty. • Knowledge of the physical properties and conditions in the Earth's crust then allows for the elucidation of regional structures that differ in their physical properties from their surroundings and that may have a common history of development with similar structures that are now hundreds of kilometers away. The Carpathian gravity low is one of the most discussed geophysical problems in the area of the Western Carpathians. The source of this regional anomaly has been debated since the 1980s. The ideas of individual authors were based on the powerful sedimentary layers in the bedrock of the flysch and Central Western Carpathians or on the effect of the source at the level of the Moho discontinuity. In 1980, the first interpretation appeared, when the authors connected the source with the presence of granitoid masses. In the course of time, individual unrealistic ideas about the influence of molassoid sediments or deep structures were gradually excluded. The work provides new interpretations based on integrated seismic, magnetotelluric (MT), and gravity data, and its conclusions are supported by the presented data and models - with limited quantitative uncertainty analysis. The study advances understanding of the Western Carpathians' crustal structure and offers a plausible geological explanation that refines long-debated hypotheses about the gravity anomaly. The results gained on the bases of the reinterpretation of gravity, magnetic, reflection seismic and magnetotelluric data (MT) confirmed the existence of an environment that can be explained by the presence of granites based on the absence of significant reflexes and the presence of high-resistivity horizons in the Low Tatras area. In this paper, compared to other similar works, a model is presented that assumes the presence of Cretaceous granitoid complexes. It is based on a comparison with a similar gravity effect manifested in the Rochovce area. Cretaceous granites drilled here proved the presence of such complexes in the subsoil in the Tatric and Veporic units. From paleographic studies, it is possible to find a connection with similar bodies of Cretaceous granites (banatites) located in the range from the Apusena Mountains to the South Carpathians. The article is devoted to the clarification of one of the important regional anomalies - Central Carpathian Gravity low", which was solved for more than 40 years by a number of expert teams. The article contains the results of geophysical methods, which offer an explanation of this structure as a source of Cretaceous granite, which is known in a large area in the Eastern and Southern Carpathians as banatites. In the article, we present a new comprehensive view of the solution of this and similar resources found in the destroyed remnants of the post-subduction Variscan zone. It is an exceptional example of possible geophysical mapping of similar zones in other orogenic regions.