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Crotone Basin

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Journal Article
Published: 01 May 2006
Journal of the Geological Society (2006) 163 (3): 471–486.
...Massimo Zecchin; Donatella Mellere; Cesare Roda Abstract Field examples from the Pliocene to Pleistocene succession of the Crotone Basin document the variability of stratal architecture in syntectonic units deposited in normal fault-bounded basins. Relatively thick trangressive intervals are common...
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Journal Article
Published: 01 October 2010
Italian Journal of Geosciences (2010) 129 (3): 353–384.
...Francesco Massari; Giacomo Prosser; Luca Capraro; Eliana Fornaciari; Chiara Consolaro Abstract The Crotone Basin, located on a stack of nappes piled up during the late Paleogene-Neogene, formed in the late Neogene to Quaternary as a forearc basin of the Ionian arc-trench system. The process of slab...
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Journal Article
Published: 01 September 2012
Journal of the Geological Society (2012) 169 (5): 613–626.
... calcite concretions associated with an extensional fault system developed in high-porosity, poorly lithified siliciclastic sediments of the Plio-Pleistocene Crotone basin, south Italy. Integration of these datasets allowed us to (1) constrain the evolution of the diagenetic environment during concretion...
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Journal Article
Journal: AAPG Bulletin
Published: 01 January 2012
AAPG Bulletin (2012) 96 (1): 155–175.
...Massimo Zecchin; Mauro Caffau Abstract The lower Pliocene shallow-marine successions deposited within half-graben subbasins exposed in the northern Crotone Basin (southern Italy) are good examples illustrating the variable development of small-scale cycles (2–15 m [6.6–49 ft] thick) within...
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Series: Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/SP285.10
EISBN: 9781862395336
... During the Messinian the sedimentation in the area was dominated by evaporitic conditions producing sulphate deposits and halite. In the Crotone basin such conditions are recorded mostly by halite (maximum thickness 300 m) and by extensive clastic evaporite deposits, such as a thick gypsarenite...
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Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.262.01.19
EISBN: 9781862395107
... that glacioeustasy may still be readable also in active tectonic settings such as that of the Crotone Basin (i.e. Rio et al . 1996 ; Massari et al . 2002 ) although tectonics and sedimentary supply are still dominant in shaping the large-scale architecture of the stratigraphic record. Above the SS, the GC...
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Journal Article
Published: 01 March 2005
Journal of Sedimentary Research (2005) 75 (2): 300–312.
...Massimo Zecchin Abstract The northern part of the Crotone Basin (southern Italy) was characterized by the activity of Pliocene growth faults bounding half-graben sub-basins. The thickest unit deposited during growth-fault activity is the lower Pliocene Belvedere Formation (up to 450 m thick), which...
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Journal Article
Published: 01 December 2003
Journal of the Geological Society (2003) 160 (6): 863–880.
...Massimo Zecchin; Francesco Massari; Donatella Mellere; Giacomo Prosser Abstract The lower Pliocene shallow-marine to continental succession of the Crotone Basin, a small forearc basin on the Calabrian Arc, Southern Italy, is represented by a mixed terrigenous–carbonate succession, up to 850 m thick...
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Journal Article
Journal: GSA Bulletin
Published: 01 October 2002
GSA Bulletin (2002) 114 (10): 1183–1209.
...F. Massari; D. Rio; M. Sgavetti; G. Prosser; A. D'Alessandro; A. Asioli; L. Capraro; E. Fornaciari; F. Tateo Abstract On a global scale, the Crotone basin preserves one of the best-developed and most complete Pleistocene marine records available in outcrop, as important as those in California, New...
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Journal Article
Published: 01 October 2008
Journal of Sedimentary Research (2008) 78 (10): 693–711.
... depozones (Rossano and Crotone basins). Sandstone assemblages have a homogeneous quartzofeldspathic composition in the Rossano and Crotone basins, characterized by a compositional trend, through time in response to regional tectonics. Evolution of the basins fill occurred during (1) Serravallian?–Tortonian...
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Sub-<b>basins</b> and structural highs in the northern <b>Crotone</b> <b>Basin</b>. ( a ) Half-g...
Published: 01 May 2006
Fig. 5.  Sub-basins and structural highs in the northern Crotone Basin. ( a ) Half-graben sub-basins active in the early Pliocene during the deposition of the Zinga 2 and Zinga 3 stratal units. NE-trending normal faults are the main structural elements of the area (modified from Zecchin et al
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( a ) Simplified geological map of the northern part of the <b>Crotone</b> <b>basin</b>, ...
Published: 01 September 2012
Fig. 1. ( a ) Simplified geological map of the northern part of the Crotone basin, south Italy (modified after Zecchin et al . 2003 ). The small black rectangle indicates the location of the studied extensional fault system and carbonate concretions. ( b ) Lithostratigraphy of the Crotone basin
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A)  Geologic sketch-map of the <b>Crotone</b> <b>Basin</b> with location of the Capo Colo...
Published: 01 October 2011
Fig. 1 A) Geologic sketch-map of the Crotone Basin with location of the Capo Colonna area, SE of Crotone (modified from M assari et alii , 2002 ); B) geologic map of the Capo Colonna promontory, with indication of the ten measured sections (modified from Z ecchin et alii , 2009 ).
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Paleomagnetic declinations from the <b>Crotone</b> <b>basin</b>. Numbers correspond to se...
Published: 01 May 2011
Figure 2. Paleomagnetic declinations from the Crotone basin. Numbers correspond to section and/or site numbers in Table 1 . Declinations from previous authors (small arrows and corresponding letters) are detailed in Table 2 .
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PALEOMAGNETIC DIRECTIONS FROM THE <b>CROTONE</b> <b>BASIN</b>
Published: 01 May 2011
TABLE 1. PALEOMAGNETIC DIRECTIONS FROM THE CROTONE BASIN
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PREVIOUS PALEOMAGNETIC DIRECTIONS FROM THE <b>CROTONE</b> <b>BASIN</b>
Published: 01 May 2011
TABLE 2. PREVIOUS PALEOMAGNETIC DIRECTIONS FROM THE CROTONE BASIN
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(A) Panoramic view of the Basilicoi section (<b>Crotone</b> <b>Basin</b>) showing the onl...
Published: 01 January 2011
Figure 15. (A) Panoramic view of the Basilicoi section (Crotone Basin) showing the onlap of the clastic evaporite unit (RLG—resedimented Lower Gypsum), including both brecciated carbonate (Calcare di Base [CdB] type 3) and gypsum, against the uppermost barren part of the Tripoli formation. (B
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Schematic columnar sections of Rossano and <b>Crotone</b> <b>basin</b> fill. Modified aft...
Published: 01 October 2008
Figure 2 Schematic columnar sections of Rossano and Crotone basin fill. Modified after Critelli (1999) and references therein. Stars and (N =) indicate studied lithostratigraphic units and number of arenite samples collected.
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A)  Location of <b>Crotone</b> <b>Basin</b> (study area);  B)  location of measured secti...
Published: 01 June 2007
Figure 1 A) Location of Crotone Basin (study area); B) location of measured sections, which crop out near the San Mauro Marchesato village.
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Geological map of the northern <b>Crotone</b> <b>Basin</b> (about 75 km 2 ), and location...
Published: 01 May 2006
Fig. 4.  Geological map of the northern Crotone Basin (about 75 km 2 ), and location of measured sections (modified from Zecchin et al . 2003 ). A–A′ corresponds to the cross-section of Figure 9 .