Substrate deformation and incorporation in sedimentary mélanges (olistostromes): Examples from the northern Apennines (Italy) and northwestern Dinarides (Slovenia)

Author:

Ogata K.,Festa A.,Pini G.A.,Pogačnik Ž.,Lucente C.C.

Funder

Ministry of Education, University and Research

Università di Parma

Università di Bologna

Università degli Studi di Trieste

Università di Torino

Publisher

Elsevier BV

Subject

Geology

Reference168 articles.

1. Multistage melange formation in the Franciscan Complex, northernmost California;Aalto;Geology,1981

2. Abbate, E., Bortolotti, V., Passerini, P. 1970. Olistostromes and olistoliths. In. Development of the Northern Apennines Geosyncline (Ed. G. Sestini), Sed. Geol., v. 4, 521–557.

3. Abbate, E., Bortolotti, V., Sagri, M.,1981. Olistostromes in the Oligocene Macigno Formation (Florence area), introduction: an approach to olistostrome interpretation. In Ricci Lucchi, F. (Ed.) International Association of Sedimentologists, 2nd European Regional Meeting, Excursion No. 5, Bologna, 1981; Excusion Guidebook, Bologna, Tecnoprint; 165–185.

4. Structure and organization of the Porma mélange: progressive denudation of a submarine nappe toe by gravitational collapse;Alonso;American Journal of Science,2006

5. Submarine slide blocks and associated soft-sediment deformation in deep-water basins. A review;Alves;Marine and Petroleum Geology,2015

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