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)

Mueller, Pierre; Tamburelli, Silvia; Menegoni, Niccolò; Perozzo, Michele; Amadori, Chiara; Crispini, Laura; Federico, Laura; Seno, Silvio; Maino, M.

doi:10.1016/j.marpetgeo.2023.106345

Cited by 6 publications

(1 citation statement)

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“…However, the seismite at the boundary between FOF and the lower member of SF is very useful for the stratigraphic correlation. The seismic pulses often directly correlate with the convergence and divergence of plates (Chen et al 2020;Laborde-Casadaban et al 2021;Mueller et al 2023). Considering the Middle Jurassic Tethys sea-floor deposition, we infer that the Middle Jurassic Gondwana breakup and synchronous active rifting (Lovecchio et al 2020) may be linked to the studied seismic pulses.…”

Section: E Implication In Region Study and Global Perspectivementioning

confidence: 61%

Linking the impact of seismicity on palaeogeographic evolution and sedimentary architecture: A case study from Middle Jurassic succession of Spiti Himalaya

Mandal,

Singh,

Banerjee

et al. 2023

Geol. Mag.

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The traces left by earthquakes in the unlithified sediments, recorded as soft-sediment deformation structures (SSDS), are well reconstructed as palaeo-seismic signals, while the origin of SSDS, seismic vs. Aseismic, is challenging. The present study discusses the origin of SSDS and its implications on palaeoceanography and sediment architecture. In the Middle Jurassic succession of Spiti Himalayan region in India, the topmost part of the Ferruginous Oolitic Formation (FOF) consists of four layers of SSDS and is underlain by the lower member of the Spiti Formation (SF). The sedimentary facies analysis documents the palaeogeographic shift from the middle shelf (carbonate-shale repository: FOF) to the outer shelf (black shale: lower member of SF). The SSDS layers, exhibiting load casts, ball and pillow structures, indicate gravitational instability, while syn-sedimentary faults and insitu breccia are the results of brittle deformation. The dominance of storms in depositional sites often argues for a possible triggering agent for SSDS. Therefore, it was necessary to distinguish between seismic vs. aseismic triggering agents. The lateral continuity, vertical repetition, confinement of SSDS at the top part of FOF and sharp change of facies assemblage indicate seismicity-induced syn-sediment deformation, i.e. seismite. The transition from middle shelf to outer shelf at the onset of seismite indicates that seismic impact possibly caused the rapid subsidence, resulting in the palaeogeographic shift. The rapid transgression is recorded as carbonate-shale repository to anoxic black shale. This study highlights the importance of sedimentological analysis to distinguish the seismite and its implications on palaeogeographic evolution and sedimentary architecture.

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Section: E Implication In Region Study and Global Perspectivementioning

confidence: 61%