2009
DOI: 10.3301/ijg.2009.128.2.257
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The geological relationships between Sardiniaand Calabria during Alpine and Hercynian times

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Cited by 3 publications
(3 citation statements)
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“…In fact, despite a similar lithological composition (Fig. 6c) and a pre-Alpine common geological history (Alvarez and Shimabukuro, 2009), CPA and SB are characterized by a very different density of polygons (0.3 polygons per squared kilometre for CPA and 1.3 for SB) due to strong differences in drafting geological sheets published almost 100 years apart from each other.…”
Section: Resultsmentioning
confidence: 99%
“…In fact, despite a similar lithological composition (Fig. 6c) and a pre-Alpine common geological history (Alvarez and Shimabukuro, 2009), CPA and SB are characterized by a very different density of polygons (0.3 polygons per squared kilometre for CPA and 1.3 for SB) due to strong differences in drafting geological sheets published almost 100 years apart from each other.…”
Section: Resultsmentioning
confidence: 99%
“…While it is not clear whether the publication year of the geological sheets plays or not a role in controlling the polygon density in the Alpine regions, the impact of the different years of publications in the representation of the regional lithological variability is dramatic comparing CPA and SB. In fact, despite a similar lithological composition (Figure 6c) and a pre-Alpine common geological history (Alvarez and Shimabukuro, 2009), CPA and SB are characterized by a very different density of polygons (0,3 polygons/km2 for CPA, and 1,3 for SB), due to strong differences in drafting geological sheets published almost 100 years apart from each other.…”
Section: Methodsmentioning
confidence: 99%
“…Dewey et al, 1989; Gueguen et al, 1997; Jolivet & Faccenna, 2000; Patacca et al, 1990; Rosenbaum & Lister, 2004; Wortel & Spakman, 2000). Since the 1960s, the Tyrrhenian Sea rift system has been the target of several geophysical and geological investigations and surveys (DSDP and ODP drilling projects in the bathyal basins) that focused on the nature of the crust (continental vs. oceanic), timing of rifting and direction of extension, faulting style (symmetrical vs. asymmetrical) (Alvarez & Shimabukuro, 2009; Florio et al, 2011; Kastens & Mascle, 1990; Lymer et al, 2018; Malinverno & Ryan, 1986; Mascle & Rehault, 1990; Milia, Iannace, et al, 2017; Milia & Torrente, 2014, 2015a, 2015b, 2018, 2022; Milia et al, 2013; Milia, Torrente, & Tesauro, 2017; Milia, Valente, et al, 2017; Nicolosi et al, 2006; Prada et al, 2014; Sartori, 1990; Sartori et al, 2001).…”
Section: Introductionmentioning
confidence: 99%