Müller, Pierre; Tamburelli, Silvia; Menegoni, Niccolò; Perozzo, Michele; Amadori, Chiara; Crispini, Laura; Federico, Laura; Seno, Silvio; Maino, Matteo:
Concurrence of Load-and-Flame Structures, Balls-and-Pillows, Clastic Injectites and Shear Deformation Bands as Indicator of Seismicity in Mixed Siliciclastic-Carbonate Successions (Finale Ligure Basin, Italy)
In: Marine and Petroleum Geology, Vol. 155 (2023), No. September, Article 106345
2023Essay / Article in JournalOpen Access
Faculty of Civil Engineering and Environmental Technology » Building materials, Geotechnical and Infrastructural Engineering Institute
Title in English:
Concurrence of Load-and-Flame Structures, Balls-and-Pillows, Clastic Injectites and Shear Deformation Bands as Indicator of Seismicity in Mixed Siliciclastic-Carbonate Successions (Finale Ligure Basin, Italy)
Author:
Müller, PierreTH Köln
DHSB-ID
THK0039941
SCOPUS
57194760725
Other
person connected with TH Köln
;
Tamburelli, Silvia
SCOPUS
57222193989
;
Menegoni, Niccolò
SCOPUS
57203386466
;
Perozzo, Michele
SCOPUS
58479283800
;
Amadori, Chiara
SCOPUS
57203394050
;
Crispini, Laura
SCOPUS
6602481105
;
Federico, Laura
SCOPUS
55957609500
;
Seno, Silvio
SCOPUS
57215529122
;
Maino, Matteo
SCOPUS
7801547449
Year of publication:
2023
„Publication Channel“:
Open Access
Scopus ID
Language of text:
English
Keyword, Topic:
Basin tectonics ; Clastic injectites ; Deformation bands ; Ligurian alps ; Load-and-flame structures ; Mediterranean basin ; Mixed siliciclastic-carbonate ; Seismites
Type of resource:
Text
Access Rights:
open access
Peer Reviewed:
Peer Reviewed
Practice Partner:
No
Category:
Research
Part of statistic:
Part of statistic

Abstract in English:

The present research explores a diverse suite of soft sediment deformation structures (SSDS) combined with clastic dykes and shear deformation bands distributed throughout a Early Miocene-age mixed carbonatesiliciclastic coastal wedge located on the Ligurian coast (NW Italy) of the Mediterranean region. The studied Aquitanian-Serravallian successions of the Finale Ligure Basin are typified by the presence of lithologically heterogeneous units, internally characterized by abrupt changes of lithofacies distributions and associated interpreted depositional environments. The interface between the terrigenous base and the carbonate wedge in many places features SSDS. Here, we report the discovery of a multiform deformational pattern, ranging from small size (cm-to dm-scale) load-and-flame structures, ball-and-pillows and mini-slumpings, to outsized (several meters in height) chaotic contorted and folded stratigraphic intervals, sand intrusions and diapir- or tree-like water escape structures. Many of the SSDS are related to fast injection of overpressurized fluids after sand liquefaction, and occur in close association with disaggregation and phyllosilicate shear bands, and sand dykelets. The stratigraphic distribution and cyclic repetitions of SSDS-prone intervals unambiguously indicates syn-depositional seismicity, thus suggesting that juxtaposition of SSDS, diapiric injectites, and shear deformation bands can serve as a suitable diagnostic criteria for seismite identification in the field. Since these particular assemblages of deformation structures reflect seismic activity in the area, they provide compelling evidence for previously undocumented tectonic episodes in Langhian-Serravallian times, associated with the latest stages of the Liguro-Provençal Basin opening.