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Fluctuating pore pressure is one important parameter for the switch between brittle and ductile deformation, thus impacting seismogenesis. Episodic tremor and slow slip events (ETS) have been proposed as a common feature of the geophysical signature of subduction zones. Their geological record, however, remains scanty. Only the detailed and further characterization of exhumed fossil geological settings can help fill this knowledge gap. Here we propose that fluctuating pore pressure linked to metamorphic dehydration reactions steered cyclic and ETS-related brittle and ductile deformation of continental crustal rocks in the subduction channel of the Apennines. Dilational shear veins and ductile mylonitic shear zones formed broadly coevally at minimum 1 GPa and 350\u00a0\u00b0C, corresponding to\u2009~\u200930\u201340\u00a0km depth in the subduction zone. We identify carpholite in Ca-poor metasediments as an important carrier of H\n                    <jats:sub>2<\/jats:sub>\n                    O to depths\u2009&gt;\u200940\u00a0km in cold subduction zones. Our results suggest that the described (micro)structures and mineralogical changes can be ascribed to deep ETS and provide a useful reference for the interpretation of similar tectonic settings worldwide.\n                  <\/jats:p>","DOI":"10.1038\/s41598-022-08489-2","type":"journal-article","created":{"date-parts":[[2022,3,16]],"date-time":"2022-03-16T09:03:10Z","timestamp":1647421390000},"update-policy":"https:\/\/doi.org\/10.1007\/springer_crossmark_policy","source":"Crossref","is-referenced-by-count":22,"title":["A likely geological record of deep tremor and slow slip events from a subducted continental broken formation"],"prefix":"10.1038","volume":"12","author":[{"given":"Francesco","family":"Giuntoli","sequence":"first","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Giulio","family":"Viola","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"297","published-online":{"date-parts":[[2022,3,16]]},"reference":[{"key":"8489_CR1","doi-asserted-by":"crossref","first-page":"329","DOI":"10.1126\/science.248.4953.329","volume":"248","author":"SM Peacock","year":"1990","unstructured":"Peacock, S. M. Fluid processes in subduction zones. Science 248, 329\u2013337 (1990).","journal-title":"Science"},{"key":"8489_CR2","doi-asserted-by":"publisher","unstructured":"Schmidt, M. W. & Poli, S. 4.19\u2014devolatilization during subduction. In (eds. Holland, H. D. & Turekian, K. K. B. T.-T. on G. 2nd ed, 669\u2013701 (Elsevier, 2014). https:\/\/doi.org\/10.1016\/B978-0-08-095975-7.00321-1.","DOI":"10.1016\/B978-0-08-095975-7.00321-1"},{"key":"8489_CR3","doi-asserted-by":"crossref","first-page":"1525","DOI":"10.1126\/science.1060152","volume":"292","author":"H Dragert","year":"2001","unstructured":"Dragert, H., Wang, K. & James, T. S. A silent slip event on the deeper cascadia subduction interface. Science 292, 1525\u20131528 (2001).","journal-title":"Science"},{"key":"8489_CR4","doi-asserted-by":"crossref","first-page":"1679","DOI":"10.1126\/science.1070378","volume":"296","author":"K Obara","year":"2002","unstructured":"Obara, K. 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