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Trappola Fault

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a ) Morphostructural characteristics of the <span class="search-highlight">Trappola</span> <span class="search-highlight">Fault</span>; the tip of whit...
Published: 01 February 2013
Fig. 13 a ) Morphostructural characteristics of the Trappola Fault; the tip of white triangles indicates the fault trace. The photo (October 2010) is taken from near the Trappola village, looking from northwest; b ) Main fault plane exposed near the Trappola village (site 17); c ) View
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The <span class="search-highlight">Trappola</span> <span class="search-highlight">Fault</span> at its northern end (October 2010):  a ) General view of...
Published: 01 February 2013
Fig. 14 The Trappola Fault at its northern end (October 2010): a ) General view of the fault at Pelago; the tip of white triangles indicates the fault trace. The white dashed lines outlines an early ca. W-verging backfold displaced by the normal fault; b ) Exhumed basal fault scarp, and c
Journal Article
Published: 01 February 2013
Italian Journal of Geosciences (2013) 132 (1): 81–97.
... master normal fault system (Trappola fault system) developed further to the East, determining the widening of the previous tectonic depression, now delimited to the North and to the South by the regional Piombino-Faenza and Arbia-Val Marecchia transfer zones, respectively. In this new tectonic depression...
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Journal Article
Published: 01 February 2013
Italian Journal of Geosciences (2013) 132 (1): 54–80.
...Fig. 13 a ) Morphostructural characteristics of the Trappola Fault; the tip of white triangles indicates the fault trace. The photo (October 2010) is taken from near the Trappola village, looking from northwest; b ) Main fault plane exposed near the Trappola village (site 17); c ) View...
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Lateral view of the northeastern margin of the Upper Valdarno Basin near Ca...
Published: 01 February 2013
the higher section of the upper sub-synthem of the Montevarchi Synthem. The bold black arrow indicates the break in topographic profile marking the transition from the Early-Middle(?) Pleistocene basin fill to the bedrock, and possibly the presence of a normal fault (sub-parallel to the Trappola fault
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Cartoon showing the tectono-sedimentary evolution hypothesized for the Uppe...
Published: 01 February 2013
propagating and/or surfacing at the base of the Chianti Mountains. The basin depocentre localised at the southwestern basin margin; c ) Development of normal faults on the northeastern basin margin (Trappola Fault), and subordinately in the central part of the basin. This phase determined the shifting
Journal Article
Published: 01 February 2013
Italian Journal of Geosciences (2013) 132 (1): 13–32.
... by an unconformity surface. These Authors provided the first structural interpretation of the basin, and recognized the main normal fault system (Trappola fault) along the NE margin. Fig. 2 Stratigraphic schemes proposed in literature for the Upper Valdarno Basin since Azzaroli & Lazzeri (1977) . See...
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Journal Article
Published: 01 February 2013
Italian Journal of Geosciences (2013) 132 (1): 137–148.
... of fluvial/alluvial systems associated to increasing tectonics (i.e. activation of Trappola fault; Bonini et alii , 2013 ) promoted very unstable palaeoenvironmental conditions unfavorable for their survival, in particular at a relict status. The progressive impoverishment of the flora marks also...
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Journal Article
Published: 01 February 2013
Italian Journal of Geosciences (2013) 132 (1): 149–166.
... to the structural setting of the basin (e.g. activity of the Trappola fault sy stem; Brogi et alii , 2013 ) were higher in the axial and eastern part of the basin (i.e. close to the depocenter) than along the Chianti margin. We can therefore speculate that soils in the Francalanci pit area formed on a surface...
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