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"general (general)"; a ; "62.2462632384275"; "0.4120500981807709" . "Mathematica"; a ; "5.253283302063791"; "5.6" . "This file contains the elastic Mogi source inversion as a function of time in day from the start of the unrest."; a ; "11.365902293120639"; "11.4" . "Santorini"; a ; "https://www.wikidata.org/wiki/Q129296" . "Mogi"; a ; "4.878048780487805"; "5.2" . "geometric figure"; a ; "3.883495145631068"; "6.0" . "column"; a ; "3.236245954692557"; "5.0" . "consists of a magma chamber"; a ; "4.580745341614906"; "5.9" . "code"; a ; "5.501618122977346"; "8.5" . "2014"; a . "Ro"; a ; "5.253283302063791"; "5.6" . "rigidity"; a ; "4.724919093851133"; "7.3" . "This RO contains the VEM code, and the application to the 2011-2012 unrest at Santorini volcanic complex."; a ; "28.713858424725824"; "28.8" . "day volume change error"; a ; "3.6490683229813663"; "4.7" . "earth sciences"; a ; "46.78766276632009"; "0.8779029250144958" . "codification"; a ; "4.724919093851133"; "7.3" . 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VEM is a code to model the temporal variation in the volume change of a magmatic source surrounded by a viscoelastic shell. The code computes the ductile deformation of a concentric viscoelastic shell surrounding a shallow magma chamber, driven by separate increases in pressure. The viscoelastic model consists of a magma chamber located at a depth, d, beneath the surface, with a radius R1. The magma chamber is surrounded by a viscoelastic shell of radius of R2-R1 and rigidity mu, embedded in an elastic half-space. The code is written in Mathematica. 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