2013
DOI: 10.1016/j.jog.2012.12.006
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A new Bouguer gravity anomaly field for the Adriatic Sea and its application for the study of the crustal and upper mantle structure

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Cited by 13 publications
(13 citation statements)
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“…To further constrain the synthetic bodies, we have also modeled the Bouguer anomaly across the same cross sections. Geometries and geophysical properties (i.e., density and magnetic susceptibility) of the synthetic bodies are constrained by geological observations and previous geophysical models (Pinna et al, 1991;Sumanovac, 2010;Tassis et al, 2013). Surface observations of Triassic gabbroid rocks in the Croatian archipelago (Pamic and Balen, 2005;Juracic et al, 2004) support the model of an extensively intruded Adriatic crust in an early rifting phase related to Tethys evolution.…”
Section: Discussionmentioning
confidence: 80%
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“…To further constrain the synthetic bodies, we have also modeled the Bouguer anomaly across the same cross sections. Geometries and geophysical properties (i.e., density and magnetic susceptibility) of the synthetic bodies are constrained by geological observations and previous geophysical models (Pinna et al, 1991;Sumanovac, 2010;Tassis et al, 2013). Surface observations of Triassic gabbroid rocks in the Croatian archipelago (Pamic and Balen, 2005;Juracic et al, 2004) support the model of an extensively intruded Adriatic crust in an early rifting phase related to Tethys evolution.…”
Section: Discussionmentioning
confidence: 80%
“…In the studied area, tomographic data (Venisti et al, 2005) suggest the presence of a high velocity volume beneath the Adriatic sea and Dinaric chain from west to east; the Bouguer anomaly ranges from −60 × 10 −5 m s −2 to 30 × 10 −5 m s −2 (Tesauro et al, 2007;Tassis et al, 2013), with the minimum values observed beneath the Dinaric chain (Fig. 3a).…”
Section: Geophysical Datamentioning
confidence: 89%
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