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![Schematic stratigraphic logs of the northern Calabria-southern Apennines (northern sector). Northern sector, Apennine Platform: AAF—Anversa degli Abruzzi Formation (Fm); ARZ—Arenarie di Zannone; CBI—Calcari Cristallini Fm; CBZ—Calcari a Briozoi a Litotamni Fm; CFR—Calcareniti a Macroforaminiferi Fm; CLI—cherty limestones; CRR—Marne con Cerrogna Fm; CUS—Cusano Fm; DBS—Dolomia Superiore Fm; DBSa—cherty dolomites; FFS—Frosinone Fm; FMO—Monaci Fm; FPJ—Pietraroja Fm; FYB—Flysch di S. Biase Fm; GOD—Macchiagodena Fm; GRS—Corniola, Verde Ammonitico e Calcari e Marne a Posidonia, Calcari Bioclastici Inferiori, Calcari Diasprigni, Maiolica Detritica, Calcari Bioclastici Superiori and Calcareniti e Calciruditi a Fucoidi Fms; GUA—Guadagnolo Member (Mb); LAF—Laga Fm; LNG—Longano Fm; MAM—marls with ammonites; MSO—Flysch del Molise Fm; OBF—Occhio del Bue succession; OFE—Orfento Fm; RIV—Mount Crivari Fm; SCA—Scaglia-type deposits; SFT—Unità Spongolitica Fm; TFI—Torre Fico succession; SWC—Jurassic–Cretaceous shallow-water carbonates; TFL—Tufillo Fm; UAM—Marne a Orbuline, and Argille a Orbulina Fms. Lagonegro-Molise Basin: AVS—Argille Varicolori Superiori Fm; MRD—Marne Rosse e Verdi di Colle Dolce Fm; MSO—Flysch del Molise Fm; PBB—Calcareniti e Calciruditi di Pietrabbondante Fm; UAM—Argille a Orbulina Fm. Apulia Platform: ASP—Argille Subappennine and Montemarano sands formations; BRY—bryozoan limestone fm; FMJ—Flysch della Majella Fm; FUC—Marne a Fucoidi Fm; GES—Gessoso-Solfifera Fm; LAP—Lama dei Peligni Flysch; LBG—limestone with bryozoa and glauconite; LCL—Lepidociclina and Cerratina cherty limestones fms; LIT—lithothamnion limestone fm; MAI—Maiolica Fm; MBL—marly limestone with reworked bryozoan unit; OFE—Orfento Fm; ORB—Orbulina limestone fm; SCA—Scaglia-type deposits; SSG—Santo Spirito Group; SWC—Jurassic–Cretaceous shallow-water carbonates (Calcari di Bari and Calcari di Altamura Fms). Wedge-top deposits: ALTG—Altavilla Group; CMU—Castilenti and Mutignano Fms; GTC—Gavignano-Gorga, and Torrice Fms; MCR—Minturno conglomerates, Campobasso conglomerates, and Rigopiano Fm. Postorogenic successions: PSO—Upper Pleistocene to present deposits. Other abbreviations: Paleoc.—Paleocene; Aqui.—Aquitanian; Burd.—Burdigalian; Lang.—Langhian; Serr.—Serravallian; Tort.—Tortonian; Mess.—Messinian; Zanc.—Zanclean; Piac.—Piacenzian; Low.—Lower; Mid.—Middle; Upp.—Upper.]()
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![Schematic stratigraphic logs of the northern Calabria-southern Apennines (central sector). Central sector, Apennine Platform: APV1—Serra della Manca Member (Mb) (Flysch della Vallimala Formation [Fm] ); APV2—Serralonga Mb (Flysch della Vallimala Fm); APV3—La Foresta Mb (Flysch della Vallimala Fm); BDSc—reworked Dolomia Superiore Fm; CBI—Calcari Cristallini Fm; CDR—Calcareniti di Recommone Fm; CUS—Cusano Fm; DBS—Dolomia Superiore Fm; FFA—Frasci Fm; FFP—Fontana Porcellara; FPJ—Pietraroja Fm; FYN—Numidian Flysch Fm; IMM—Calciruditi e Calcareniti del Limmo Fm; LNG—Longano Fm; MNM—Calcari e Dolomie con selce dei Monti Mai Fm; REC—Calcareniti di Recommone Fm; RIV—Mount Crivari Fm; RTDc—reworked Calcari a Radioliditi Fm; SCA—Scaglia-type deposits; SCAd—Scaglia Detritica–type deposits; SWC—Jurassic–Cretaceous shallow-water carbonates; TMI—Arenarie di Termini Fm; TNS—Conglomerati Calcarei di Tuoro Maleconsiglio; TRN—Trentinara Fm. Lagonegro-Molise Basin: AVF—Argille Varicolori del Fortore Fm; AVG—Argille Varicolori with gypsum; CPA—Corleto Perticara Fm; FAE—Faeto Fm; FYN—Numidian Flysch Fm; FYR—Flysch Rosso Fm; PNU—post-Numidian succession; SER—Serroni Fm; SFN—Serra Funaro Fm; SGG—San Giorgio Fm; SID—Mount Sidone Fm; TPC—Toppo Capuana Fm; TUT—Tufiti di Tusa Fm. Apulian Platform: ANR—Calcareniti di Andrano Fm; ARM—clay and marl of buried outer Apulian carbonate platform; ASP—Argille Subappennine and Montemarano sands formations; BCG—Breccia di Cagnano Fm; CTT—Calcari di Trombetta, Brecce e Conglomerati di Stazione S. Giacomo and Calcari di Fiumicello Fms; DBS—Dolomia Superiore Fm; FUC—Marne a Fucoidi Fm; GAR1—shales, dolostones, and limestones; GAR2—sandstones, dolostones, and limestones; GRA—Calcareniti di Gravina Fm; GES—Gessoso-Solfifera Fm; LAP—Lama dei Peligni Flysch; LAV—Brecce di Lavello Fm; MAI—Maiolica Fm; PES—Peschici Fm; PLE—Pietra Leccese Fm; SCA—Scaglia-type deposits; CAd—Scaglia Detritica–type deposits; SMH—Calcari di Grotta San Michele Fm; SWC—Jurassic–Cretaceous shallow-water carbonates (Calcari di Bari and Calcari di Altamura Fms); TPL—Tripoli Fm; TRF—Torre Rossa Fm. Wedge-top deposits: CVTG—Castelvetere Group; ALTG—Altavilla Group; BAR—Baronia Fm; SFE—Sferracavallo Fm. Postorogenic successions: PSO—Upper Pleistocene to present deposits. Other abbreviations: Paleoc.—Paleocene; Aqui.—Aquitanian; Burd.—Burdigalian; Lang.—Langhian; Serr.—Serravallian; Tort.—Tortonian; Mess.—Messinian; Zanc.—Zanclean; Piac.—Piacenzian; Low.—Lower; Mid.—Middle; Upp.—Upper.]()
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![Schematic stratigraphic logs of the northern Calabria-southern Apennines (southern sector). Southern sector, Calabria-Peloritani terrane: CAL—Caloveto and Longobucco groups; CML—cherty meta-limestone; PAL—Paleozoic basement; PSV—Pseudo-Verrucano Formation (Fm). Ligurian Ocean: ALB—Albanella Fm; AVI—Argille Varicolori Inferiori Fm; AVS—Argille Varicolori Superiori Fm; CAR—Mount Caramola Fm; CON—Contursi Fm; CRN—Crete Nere Fm; EPM—Episcopia mélange; FMS—Mount Sant’Arcangelo Fm; MSC—undifferentiated metasedimentary cover; MTB—undifferentiated metabasalts; NRV—Noce River Valley mélange; POS—Postiglione Fm; SAR—Saraceno Fm; SOV—Sovereto Fm; SSL—S. Severino Lucano Fm; TLG—Tempa La Guardia Fm; TRO—Tempa Rotalupo Fm; TUT—Tufiti di Tusa–Arenarie di Corleto Fms. Apennine Platform: BIF—Bifurto Fm; CBI—Calcari Cristallini Fm; CDO—cherty dolomites; CIA—slope limestones of Pollino-Ciagola Unit; CLI—cherty limestone; DBS—Dolomia Superiore Fm; FCE—Cerchiara Fm; FLB1—Alberosa Fm (Brecce Poligeniche member [mb]); FLB2—Alberosa Fm (Calcari a Nummiliti mb); FLB3—Alberosa Fm (Serra Costantino mb); FOP—Dolomie e Calcari di Monte Foraporta Fm; FYN—Numidian Flysch Fm; GIP—Argilliti e Calcari di S. Giovanni a Piro Fm; LAV—Laviano marls, calcarenites, and sandstones; MRA—meta-radiolarites; PMM—phyllites, meta-limestones, and metarenites; RCG—Calcari e Argilliti di Roccagloriosa Fm; SCA—Scaglia-type deposits; SCAd—Scaglia Detritica–type deposits; FL—Scisti del F. Lao Fm; CET—Cetraro Unit; SWC—Jurassic–Cretaceous shallow-water carbonates; TRN—Trentinara Fm. Lagonegro-Molise Basin: AVG—Argille Variegate Fm; CPA—Corleto Perticara Fm; FAC—Monte Facito Fm; FAE—Faeto Fm; FYG—Flysch Galestrino Fm; FYN—Numidian Flysch Fm; FYR—Flysch Rosso Fm; PAA—Serra Palazzo Fm; PDO—Paola Doce Fm; PNU—post-Numidian succession; SGG—San Giorgio Fm; SLC—Calcari con Selce Fm; STS—Scisti Silicei Fm; TFA—Torrente Flaga Fm. Apulian Platform: ALT1—Calcare del Ciolo mb (Calcare di Altamura Fm); ANR—Calcareniti di Andrano Fm; ARM—clay and marl of buried outer Apulian Platform; ASP—Argille Subappennine and Montemarano sands Fms; BLA—Brecce di Lavello Fm; BSM—Calcarenite Coralligena di Serra del Mito Fm; CSR—Calcare di Castro Fm; DBS—Dolomia Superiore Fm; GES—Gessoso-Solfifera Fm; LAP—Lama dei Peligni Flysch; LUT—Calcareniti di Cava Iannazzo; PBD—Calcareniti di Porto Badisco Fm; PLE—Pietra Leccese Fm; PUG1—sandstones; PUG2—breccias; SCA—Scaglia-type deposits; SWC—Jurassic–Cretaceous shallow-water carbonates (Calcari di Bari and Calcari di Altamura Fms); TIT—Conglomerati e Arenarie di Cima S. Croce; TTG—Calcare di Torre Tiggiano; TRB—Trubi Fm; UGC—Uggiano La Chiesa Fm. Wedge-top deposits: ABD—Albidona Fm (CIG); ALTG—Altavilla Group; AMA—Amantea; ARC—S. Arcangelo Basin deposits; BAR—Baronia Fm; CVTG—Castelvetere Group; MAU—S. Mauro Fm (CIG); PLU—Paludi Fm; PER—Perosa Fm; POL—Pollica Fm (CIG); ROS—Rossano basin deposits; SFE—Sferracavallo Fm. Postorogenic successions: PSO—Upper Pleistocene to present deposits. Metamorphic ages: M1—Castagna Unit (Schenk, 1980); M2—Gimigliano Unit (Rossetti et al., 2001, 2004); M3—Diamante-Terranova Unit (Shimabukuro et al., 2012); M4—Cetraro Unit (Iannace et al., 2007). Thermochronologic ages: Castagna and Bagni Units—FT1 zircon fission tracks (Thomson, 1998), FT2 apatite fission tracks (Thomson, 1998); Lungro-Verbicaro Unit—FT3 apatite fission tracks (Iannace et al., 2007); Lagonegro I and II Units—FT4 apatite fission tacks (Mazzoli et al., 2008); M. Alpi—FT5 apatite fission tracks (Mazzoli et al., 2006). Other abbreviations: Paleoc.—Paleocene; Aqui.—Aquitanian; Burd.—Burdigalian; Lang.—Langhian; Serr.—Serravallian; Tort.—Tortonian; Mess.—Messinian; Zanc.—Zanclean; Piac.—Piacenzian; Low.—Lower; Mid.—Middle; Upp.—Upper.]()
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1-20 OF 51 RESULTS FOR
Gessoso Solfifera Group
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1
Journal Article
Carbonate replacements after sulfate evaporites in the middle Miocene of Egypt Available to Purchase
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
Published: 01 May 1988
Journal of Sedimentary Research (1988) 58 (3): 446–456.
..., and stable isotope composition to diagenetic carbonates described in some portions of Messinian "Gessoso Solfifera" Formation of Sicily and in the "Castiles" of the Upper Permian Castile Formation of the Delaware basin. The mechanism of mineral transformation is basically bacterial sulfate reduction because...
Journal Article
Sedimentary and tectonic evolution of the Vena del Gesso basin (Northern Apennines, Italy): Implications for the onset of the Messinian salinity crisis Available to Purchase
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 April 2003
GSA Bulletin (2003) 115 (4): 387–405.
.... The Gessoso-solfifera Formation (Messinian), is made up of both primary and clastic, resedimented evaporites with interbedded organic-rich shales, deposited during the evaporitic and postevaporitic stages of the Messinian salinity crisis. 3. The Colombacci Formation (upper Messinian), consisting...
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Journal Article
Geological map of the Corvillo and Mandre Basins (Caltanissetta Basin, Central Sicily): Explanatory notes Available to Purchase
Journal: Italian Journal of Geosciences
Publisher: Societa Geologica Italiana
Published: 01 June 2010
Italian Journal of Geosciences (2010) 129 (2): 316–326.
... of quartzarenites and Mesozoic carbonate clasts. Maximum thickness 100 m. The Gessoso-Solfifera Group deposits are the most widespread deposits in Corvillo and Mandre basins both at outcrop and in the subsurface. They are divided into two formations (Cattolica and Pasquasia Formations): the Lower...
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Journal Article
The Mediterranean water body in the late Messinian: interpreting the record from marginal basins on Sicily Available to Purchase
Journal: Journal of the Geological Society
Publisher: Geological Society of London
Published: 01 August 1999
Journal of the Geological Society (1999) 156 (4): 837–846.
... 1993; Pedley 1996). The lower Messinian is marked by the regionally regressive carbonates of the Calcare di Base and so-called First Cycle evaporites. These form the lower part of the Gessoso Solfifera Formation (Ogniben 1957). These pri- mary evaporites are in turn unconformably overlain...
Journal Article
Stratigraphic and structural reconstruction of an offshore sector of the Hyblean Foreland ramp (southern Italy) Available to Purchase
Journal: Italian Journal of Geosciences
Publisher: Societa Geologica Italiana
Published: 01 October 2019
Italian Journal of Geosciences (2019) 138 (3): 390–403.
... and down-faulted sectors. These faults are inferred to record the early history of the Scicli Line and of the polyphase kinematic evolution of the N50° oriented regional fault systems. The Gessoso-Solfifera deposits (Messinian, Late Miocene) have been recognized in several sectors of the study area...
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Journal Article
Hydrocarbon-Bearing Submarine Fan System of Cellino Formation, Central Italy Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 March 1983
AAPG Bulletin (1983) 67 (3): 359–370.
...; solid circles are wells cited in text and in figures. Cenozoic-Mesozoic limestones include carbonate successions up to middle Miocene. Upper Miocene includes Laga and “Gessoso-solfifera” Formations; latter is developed mainly on south of mapped area. Limits between Laga and Cellino Formations...
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Journal Article
Evidence for active El Niño Southern Oscillation variability in the Late Miocene greenhouse climate Available to Purchase
Journal: Geology
Publisher: Geological Society of America
Published: 01 May 2010
Geology (2010) 38 (5): 419–422.
... halovarve thickness record with those of the modern ENSO and NAO, and run a fully coupled climate model simulation to investigate the extent of Miocene ENSO teleconnections relative to today. The halovarves comes from the Gesso balatino facies of the Gessoso Solfifera formation, deposited during...
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Journal Article
An outline of the geology of the Northern Apennines (Italy), with geological map at 1:250,000 scale Available to Purchase
Journal: Italian Journal of Geosciences
Publisher: Societa Geologica Italiana
Published: 01 June 2020
Italian Journal of Geosciences (2020) 139 (2): 149–194.
...), to evaporite gypsum and bituminous muds (Gessoso-solfifera Fm., mapped as MI gs ). The complete stratigraphic record of the T2 sequence is formed, from bottom to top: Acquaviva Fm. and Termina Fm., Casa i Gessi Clays, Gessoso-solfifera Fm. ( R icci L ucchi , 1986 ; C atanzariti et alii , 2002 ; C...
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Includes: Supplemental Content
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Schematic stratigraphic logs of the northern Calabria-southern Apennines (n... Available to Purchase
in Orogenic evolution of the northern Calabria–southern Apennines system in the framework of the Alpine chains in the central-western Mediterranean area
> GSA Bulletin
Published: 27 September 2024
Dolce Fm; MSO—Flysch del Molise Fm; PBB—Calcareniti e Calciruditi di Pietrabbondante Fm; UAM—Argille a Orbulina Fm. Apulia Platform: ASP—Argille Subappennine and Montemarano sands formations; BRY—bryozoan limestone fm; FMJ—Flysch della Majella Fm; FUC—Marne a Fucoidi Fm; GES—Gessoso-Solfifera Fm; LAP
Journal Article
Testing thrust tectonic models at mountain fronts: where has the displacement gone? Available to Purchase
Journal: Journal of the Geological Society
Publisher: Geological Society of London
Published: 01 January 2006
Journal of the Geological Society (2006) 163 (1): 1–14.
... thickness of the Laga Formation is almost 3000 m ( Vezzani & Ghisetti 1998 ), whereas coeval shales and gypsum deposited on the foredeep margin (Gessoso-solfifera Formation) are <100 m thick. These are penetrated by wells beneath the Adriatic Sea to the east, and in the Marche region to the north...
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Image
![Schematic stratigraphic logs of the northern Calabria-southern Apennines (central sector). Central sector, Apennine Platform: APV1—Serra della Manca Member (Mb) (Flysch della Vallimala Formation [Fm] ); APV2—Serralonga Mb (Flysch della Vallimala Fm); APV3—La Foresta Mb (Flysch della Vallimala Fm); BDSc—reworked Dolomia Superiore Fm; CBI—Calcari Cristallini Fm; CDR—Calcareniti di Recommone Fm; CUS—Cusano Fm; DBS—Dolomia Superiore Fm; FFA—Frasci Fm; FFP—Fontana Porcellara; FPJ—Pietraroja Fm; FYN—Numidian Flysch Fm; IMM—Calciruditi e Calcareniti del Limmo Fm; LNG—Longano Fm; MNM—Calcari e Dolomie con selce dei Monti Mai Fm; REC—Calcareniti di Recommone Fm; RIV—Mount Crivari Fm; RTDc—reworked Calcari a Radioliditi Fm; SCA—Scaglia-type deposits; SCAd—Scaglia Detritica–type deposits; SWC—Jurassic–Cretaceous shallow-water carbonates; TMI—Arenarie di Termini Fm; TNS—Conglomerati Calcarei di Tuoro Maleconsiglio; TRN—Trentinara Fm. Lagonegro-Molise Basin: AVF—Argille Varicolori del Fortore Fm; AVG—Argille Varicolori with gypsum; CPA—Corleto Perticara Fm; FAE—Faeto Fm; FYN—Numidian Flysch Fm; FYR—Flysch Rosso Fm; PNU—post-Numidian succession; SER—Serroni Fm; SFN—Serra Funaro Fm; SGG—San Giorgio Fm; SID—Mount Sidone Fm; TPC—Toppo Capuana Fm; TUT—Tufiti di Tusa Fm. Apulian Platform: ANR—Calcareniti di Andrano Fm; ARM—clay and marl of buried outer Apulian carbonate platform; ASP—Argille Subappennine and Montemarano sands formations; BCG—Breccia di Cagnano Fm; CTT—Calcari di Trombetta, Brecce e Conglomerati di Stazione S. Giacomo and Calcari di Fiumicello Fms; DBS—Dolomia Superiore Fm; FUC—Marne a Fucoidi Fm; GAR1—shales, dolostones, and limestones; GAR2—sandstones, dolostones, and limestones; GRA—Calcareniti di Gravina Fm; GES—Gessoso-Solfifera Fm; LAP—Lama dei Peligni Flysch; LAV—Brecce di Lavello Fm; MAI—Maiolica Fm; PES—Peschici Fm; PLE—Pietra Leccese Fm; SCA—Scaglia-type deposits; CAd—Scaglia Detritica–type deposits; SMH—Calcari di Grotta San Michele Fm; SWC—Jurassic–Cretaceous shallow-water carbonates (Calcari di Bari and Calcari di Altamura Fms); TPL—Tripoli Fm; TRF—Torre Rossa Fm. Wedge-top deposits: CVTG—Castelvetere Group; ALTG—Altavilla Group; BAR—Baronia Fm; SFE—Sferracavallo Fm. Postorogenic successions: PSO—Upper Pleistocene to present deposits. Other abbreviations: Paleoc.—Paleocene; Aqui.—Aquitanian; Burd.—Burdigalian; Lang.—Langhian; Serr.—Serravallian; Tort.—Tortonian; Mess.—Messinian; Zanc.—Zanclean; Piac.—Piacenzian; Low.—Lower; Mid.—Middle; Upp.—Upper.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/gsabulletin/137/3-4/10.1130_B37474.1/4/s_b37474.1_f05.png?Expires=2147483647&Signature=lIaV5dG6506YnwFh711auyAE-QQCs5tP0vbIAAVxYOJgWbPeYvC8FhaP5Tk6QZGxqBUq~yF5OVm4t5G6eMA86EOiJWdhAVvfZQzFaXYgl59qxkzE6rJfIWIlZl8SSXTlIBeawInhHgrtrtM8mDLcUzL8Nxn6OHhmVFgbLG4v5wrG-~-zqCK4Ike4Rp3aFt0msSv924ThtqCGit8LEpQwB1spkIt5vmebeE3JogZIP2Ffg9icBxZyYrmC0uwlj8SZ2XIXdm9xMxeOm~TNdLDkMrfcj9K0Ah2tTJJiiEA83tPxeqMwg~E9krdTR0u2F9~2n4Hbs4wVUm516l27-AJ~xQ__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Schematic stratigraphic logs of the northern Calabria-southern Apennines (c... Available to Purchase
in Orogenic evolution of the northern Calabria–southern Apennines system in the framework of the Alpine chains in the central-western Mediterranean area
> GSA Bulletin
Published: 27 September 2024
, Brecce e Conglomerati di Stazione S. Giacomo and Calcari di Fiumicello Fms; DBS—Dolomia Superiore Fm; FUC—Marne a Fucoidi Fm; GAR1—shales, dolostones, and limestones; GAR2—sandstones, dolostones, and limestones; GRA—Calcareniti di Gravina Fm; GES—Gessoso-Solfifera Fm; LAP—Lama dei Peligni Flysch; LAV
Journal Article
Orbitally forced paleoenvironmental and paleoclimate changes in the late postevaporitic Messinian of the central Mediterranean Basin Available to Purchase
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 March 2012
GSA Bulletin (2012) 124 (3-4): 499–516.
... Peligna and Lama dei Peligni. At the Taranta Peligna cemetery, the base of the Lago-Mare clays conformably rests on resedimented gypsum deposits (“Gessoso-solfifera” Formation). These resedimented gypsum deposits unconformably overlie the lower Messinian marls with Turborotalia multiloba ( Fig. 1C...
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Journal Article
3D modelling of the Tremiti salt diapir in the Gargano offshore (Adriatic Sea, southern Italy): constraints on the Tremiti Structure development Available to Purchase
Journal: Italian Journal of Geosciences
Publisher: Societa Geologica Italiana
Published: 01 October 2016
Italian Journal of Geosciences (2016) 135 (3): 474–485.
... reflections of the Gessoso-Solfifera Fm; Unit C comprises middle Lias to lower Messinian lithostratigraphic units corresponding to the pelagic Adriatic Basin succession. Finally, Unit D is characterized by some continuous reflections, and, locally, by semi-transparent seismic facies; internal unconformities...
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Journal Article
The Integrated Plant Record: An Essential Tool For Reconstructing Neogene Zonal Vegetation In Europe Available to Purchase
Journal: PALAIOS
Publisher: SEPM Society for Sedimentary Geology
Published: 01 February 2008
PALAIOS (2008) 23 (2): 97–111.
... interpretation. For the pollen record from the Salt Member of the Gessoso-Solfifera Formation (locality nos. 952–954; Fig. 2 ; Supplementary Data 3 1 ), however, the interpretations are closer, that is, open woodlands or xerophyllous forests in the current study and open vegetation in Bertini et al. (1998...
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Journal Article
Biostratigraphic and palaeoenvironmental analyses of the Messinian/Zanclean boundary and Zanclean succession in the Moncucco quarry (Piedmont, northwestern Italy) Available to Purchase
Publisher: Société Géologique de France
Published: 01 March 2011
Bulletin de la Société Géologique de France (2011) 182 (2): 149–162.
... ). – Il Messiniano Piemontese: nuovi dati su due aree campione . – PhD Thesis , Università di Torino , 167 p Irace A. , Dela Pierre F. & Clari P. ( 2005 ). – “Normal” and “chaotic” deposits in the Messinian Gessoso Solfifera formation at the northeastern border...
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![Schematic stratigraphic logs of the northern Calabria-southern Apennines (southern sector). Southern sector, Calabria-Peloritani terrane: CAL—Caloveto and Longobucco groups; CML—cherty meta-limestone; PAL—Paleozoic basement; PSV—Pseudo-Verrucano Formation (Fm). Ligurian Ocean: ALB—Albanella Fm; AVI—Argille Varicolori Inferiori Fm; AVS—Argille Varicolori Superiori Fm; CAR—Mount Caramola Fm; CON—Contursi Fm; CRN—Crete Nere Fm; EPM—Episcopia mélange; FMS—Mount Sant’Arcangelo Fm; MSC—undifferentiated metasedimentary cover; MTB—undifferentiated metabasalts; NRV—Noce River Valley mélange; POS—Postiglione Fm; SAR—Saraceno Fm; SOV—Sovereto Fm; SSL—S. Severino Lucano Fm; TLG—Tempa La Guardia Fm; TRO—Tempa Rotalupo Fm; TUT—Tufiti di Tusa–Arenarie di Corleto Fms. Apennine Platform: BIF—Bifurto Fm; CBI—Calcari Cristallini Fm; CDO—cherty dolomites; CIA—slope limestones of Pollino-Ciagola Unit; CLI—cherty limestone; DBS—Dolomia Superiore Fm; FCE—Cerchiara Fm; FLB1—Alberosa Fm (Brecce Poligeniche member [mb]); FLB2—Alberosa Fm (Calcari a Nummiliti mb); FLB3—Alberosa Fm (Serra Costantino mb); FOP—Dolomie e Calcari di Monte Foraporta Fm; FYN—Numidian Flysch Fm; GIP—Argilliti e Calcari di S. Giovanni a Piro Fm; LAV—Laviano marls, calcarenites, and sandstones; MRA—meta-radiolarites; PMM—phyllites, meta-limestones, and metarenites; RCG—Calcari e Argilliti di Roccagloriosa Fm; SCA—Scaglia-type deposits; SCAd—Scaglia Detritica–type deposits; FL—Scisti del F. Lao Fm; CET—Cetraro Unit; SWC—Jurassic–Cretaceous shallow-water carbonates; TRN—Trentinara Fm. Lagonegro-Molise Basin: AVG—Argille Variegate Fm; CPA—Corleto Perticara Fm; FAC—Monte Facito Fm; FAE—Faeto Fm; FYG—Flysch Galestrino Fm; FYN—Numidian Flysch Fm; FYR—Flysch Rosso Fm; PAA—Serra Palazzo Fm; PDO—Paola Doce Fm; PNU—post-Numidian succession; SGG—San Giorgio Fm; SLC—Calcari con Selce Fm; STS—Scisti Silicei Fm; TFA—Torrente Flaga Fm. Apulian Platform: ALT1—Calcare del Ciolo mb (Calcare di Altamura Fm); ANR—Calcareniti di Andrano Fm; ARM—clay and marl of buried outer Apulian Platform; ASP—Argille Subappennine and Montemarano sands Fms; BLA—Brecce di Lavello Fm; BSM—Calcarenite Coralligena di Serra del Mito Fm; CSR—Calcare di Castro Fm; DBS—Dolomia Superiore Fm; GES—Gessoso-Solfifera Fm; LAP—Lama dei Peligni Flysch; LUT—Calcareniti di Cava Iannazzo; PBD—Calcareniti di Porto Badisco Fm; PLE—Pietra Leccese Fm; PUG1—sandstones; PUG2—breccias; SCA—Scaglia-type deposits; SWC—Jurassic–Cretaceous shallow-water carbonates (Calcari di Bari and Calcari di Altamura Fms); TIT—Conglomerati e Arenarie di Cima S. Croce; TTG—Calcare di Torre Tiggiano; TRB—Trubi Fm; UGC—Uggiano La Chiesa Fm. Wedge-top deposits: ABD—Albidona Fm (CIG); ALTG—Altavilla Group; AMA—Amantea; ARC—S. Arcangelo Basin deposits; BAR—Baronia Fm; CVTG—Castelvetere Group; MAU—S. Mauro Fm (CIG); PLU—Paludi Fm; PER—Perosa Fm; POL—Pollica Fm (CIG); ROS—Rossano basin deposits; SFE—Sferracavallo Fm. Postorogenic successions: PSO—Upper Pleistocene to present deposits. Metamorphic ages: M1—Castagna Unit (Schenk, 1980); M2—Gimigliano Unit (Rossetti et al., 2001, 2004); M3—Diamante-Terranova Unit (Shimabukuro et al., 2012); M4—Cetraro Unit (Iannace et al., 2007). Thermochronologic ages: Castagna and Bagni Units—FT1 zircon fission tracks (Thomson, 1998), FT2 apatite fission tracks (Thomson, 1998); Lungro-Verbicaro Unit—FT3 apatite fission tracks (Iannace et al., 2007); Lagonegro I and II Units—FT4 apatite fission tacks (Mazzoli et al., 2008); M. Alpi—FT5 apatite fission tracks (Mazzoli et al., 2006). Other abbreviations: Paleoc.—Paleocene; Aqui.—Aquitanian; Burd.—Burdigalian; Lang.—Langhian; Serr.—Serravallian; Tort.—Tortonian; Mess.—Messinian; Zanc.—Zanclean; Piac.—Piacenzian; Low.—Lower; Mid.—Middle; Upp.—Upper.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/gsabulletin/137/3-4/10.1130_B37474.1/4/s_b37474.1_f04.png?Expires=2147483647&Signature=gKUGg6jehLtNNoAIPc-GYjwCjdl7UxNpIugx7rVIiG8ppi~K0KmmwZUyV6ftylyWMVzxDR4So1yYmIKXpDqMSERBpA653biO8Oj1I6cZY3atHJ-bXSFSn6vR~FCvXk49byG~oJijMhPa2JWvKLjuObimVcR9iE70iizMGhrdlkhdjI18fDT27WpL82xb4WPMv8wbu4gD9ANqF1zbGsy9xPpuQYdrUD7V754ZM0JM~sGsj-P0J-zaIQvB-ZHsmLrYgO1qxPI-3fB5Syhko7C~wVzNr6VMRu~63qreUIvjTbapdPMeUI01yCWVEoqOf2EXQdqU~2vvQDjLl6dR2wU1ng__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Schematic stratigraphic logs of the northern Calabria-southern Apennines (s... Available to Purchase
in Orogenic evolution of the northern Calabria–southern Apennines system in the framework of the Alpine chains in the central-western Mediterranean area
> GSA Bulletin
Published: 27 September 2024
—Brecce di Lavello Fm; BSM—Calcarenite Coralligena di Serra del Mito Fm; CSR—Calcare di Castro Fm; DBS—Dolomia Superiore Fm; GES—Gessoso-Solfifera Fm; LAP—Lama dei Peligni Flysch; LUT—Calcareniti di Cava Iannazzo; PBD—Calcareniti di Porto Badisco Fm; PLE—Pietra Leccese Fm; PUG1—sandstones; PUG2—breccias
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From seismic to bed: surface–subsurface correlations within the turbiditic Cellino Formation (central Italy) Available to Purchase
Journal: Petroleum Geoscience
Publisher: Geological Society of London
Published: 01 April 2004
Petroleum Geoscience (2004) 10 (2): 131–140.
...) of the Cellino Formation lies on the Messinian Colombacci Formation (shales with sandstones and subordinate gypsiferous beds), or on sandstone–shale beds (Teramo Flysch). East of the Villadegna 1 well, the evaporites (gypsum) of the Gessoso–Solfifera Formation can be found under the Colombacci Formation...
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Astronomical dating of two Pliocene alkaline volcanic ash layers in the Capo Rossello area (southern Sicily, Italy): implications for the beginning of the rifting in the Sicily Channel Available to Purchase
Publisher: Société Géologique de France
Published: 01 March 2009
Bulletin de la Société Géologique de France (2009) 180 (2): 95–104.
.... Samples are mostly dominated by clay minerals, quartz and gypsum, very often dehydrated to hemi-hydrate (CaSO 4 *0.5H 2 O) during sample preparation (fig. 5-a-b-c ). Gypsum easily crystallises from high sulphatic groundwaters that interact with evaporitic sediments of Messinian Gessoso-Solfifera Formation...
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Geology and Cultural Heritage: characterization and provenance of local stones and spolia used in the Romanesque façade of Santa Maria della Piazza church (Ancona, Central Italy) Available to Purchase
Journal: Italian Journal of Geosciences
Publisher: Societa Geologica Italiana
Published: 01 October 2020
Italian Journal of Geosciences (2020) 139 (3): 451–468.
... Gessina was detected in the wall of the lower part of the façade ( Figs.1 , 3 ) with its typical black colour. This stone belongs to the Gessoso-Solfifera Formation (Messinian p.p.) outcropping, with a thickness up to 100 m, in the Aliforni - San Severino Basin ( D eiana , 2009 ) at about 60 km...
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Geologic Framework of Italian Petroleum Resources Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 February 1986
AAPG Bulletin (1986) 70 (2): 103–130.
... throughout the Mediterranean and the concomitant emergence of vast areas. The typical sequence of these deposits is that of the Gessoso-Solfifera Formation: Tripoli Formation, sulfurbearing limestone, and gypsum. In the Po plain subsurface ( Rizzini and Dondi, 1979 ) and in the northern Apennines...
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