Abstract
In this study we combine observations and analytical data from large-scale (10–100s of m-thick and 100 m2-extensive), siliciclastic and carbonate MTD/MTCs belonging to the Oligocene – Miocene foredeep and wedge-top successions of the Northern Apennines and the Paleocene – Eocene Friuli basin of the northwestern Dinarides (Italy and Slovenia), to discuss the deformation processes critical to the emplacement of submarine landslides. We focus on the identification of meso-scale structures, used as diagnostic kinematic indicators of local paleo-transport directions. These structures, represented by linear-planar and complex-shaped elements such as tabular shear zones and detached slump-type folds, are the product of ductile-plastic deformation developed at relatively low-confining pressure that involves water-saturated, un- to poorly-lithified sediments, along with liquefaction/fluidization processes. Their final appearance is thus mainly controlled by the mechanical-rheological behavior of deformed sediments, and eventually by tectonic fabrics inherited from deeper structural levels of deformation. Due to this parallelism these structures have been termed and classified accordingly. They reflect strain partitioning due to differential movements within the slide mass, which is in turn controlled by the overall landslide typology. Due to the parallelism with classified tectonic structures and structural associations, we have thus redefined and classified accordingly meso-scale kinematic indicators in ancient MTD/MTCs.
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References
Alonso JL, Marcos A, Suàrez A (2006) Structure and organization of the Porma mélange: progressive denudation of a submarine nappe toe by gravitational collapse. Am J Sci 306:32–65
Kawamura K, Sasaki T, Kanamatsu Y, Sakaguchi A, Ogawa Y (2012) Large submarine landslides in the Japan trench: a new scenario for additional tsunami generation. Geophys Res Lett 39:L05308. doi:10.1029/2011GL050661
Lucente CC (2004) Topography and palaeogeographic evolution of a middle Miocene foredeep basin plain (Northern Apennines, Italy). Sediment Geol 170:107–134
Lucente CC, Pini GA (2003) Anatomy and emplacement mechanism of a large submarine slide within the Miocene foredeep in the Northern Apennines, Italy: a field perspective. Am J Sci 303:565–602
Ogata K, Mutti E, Tinterri R, Pini GA (2012) Mass transport-related stratal disruption within sedimentary mélanges. Tectonophysics 568–569:185–199
Ogata K, Pogačnik Ž, Pini GA, Tunis G, Festa A, Camerlenghi A, Rebesco M (2014) The carbonate mass transport deposits of the Paleogene Julian-Slovenian Basin (Italy/Slovenia): internal anatomy and inferred genetic processes. Mar Geol 356:88–110
Passchier CW, Trouw RA (2005) Microtectonics. Springer, Berlin
Pini GA, Ogata K, Camerlenghi A, Festa A, Lucente CC, Codegone G (2012) Sedimentary mélanges and fossil mass-transport complexes: a key for better understanding submarine mass movements? In: Yamada Y et al (eds) Submarine mass movements and their consequences: advances in natural and technological hazards research, vol 31. Springer, Berlin
Strasser M, Moore GF, Kimura G, Kopf AJ, Underwood MB, Guo J, Screaton EJ (2011) Slumping and mass transport deposition in the Nankai fore arc: evidence from IODP drilling and 3‐D reflection seismic data. Geochem Geophys Geosyst 12:1–24. doi:10.1029/2010GC003431
Yamamoto Y, Nidaira M, Ohta Y, Ogawa Y (2009) Formation of chaotic rock units during primary accretion processes: examples from the Miura-Boso accretionary complex, central Japan. Island Arc 18:496–512
Acknowledgements
We are grateful to the associate editor Christof Mueller, and the reviewers Yuzuru Yamamoto and Juan Luis Alonso for their helpfulness and their constructive feedbacks. This work is funded by the FRA2013 research grants of the Università di Trieste and MIUR PRIN grant 2010AZR98L_002.
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Ogata, K., Pini, G.A., Festa, A., Pogačnik, Ž., Lucente, C.C. (2016). Meso-Scale Kinematic Indicators in Exhumed Mass Transport Deposits: Definitions and Implications. In: Lamarche, G., et al. Submarine Mass Movements and their Consequences. Advances in Natural and Technological Hazards Research, vol 41. Springer, Cham. https://doi.org/10.1007/978-3-319-20979-1_46
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DOI: https://doi.org/10.1007/978-3-319-20979-1_46
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