applying 2d algorithms for inverting the potential field data is more useful and efficient than their 3d counterparts, whenever the geologic situation permits. this is because the computation time is less and modeling the subsurface is easier. in this paper we present a 2d inversion algorithm for interpreting gravity data by employing a set of constraints including minimum distance, smoothness,...

Abstract For a graph G , and two distinct vertices u v of let $$n_{G}(u,v)$$ n G ( u , v ) be the number that are closer in to than . Miklavi? Šparl (arXiv:2011.0...