38 citations as recorded by crossref.

1. Are repetitive slumpings during sapropel S1 related to paleo-earthquakes? A. Polonia et al. 10.1016/j.margeo.2015.01.001
2. Which earthquakes trigger damaging submarine mass movements: Insights from a global record of submarine cable breaks? E. Pope et al. 10.1016/j.margeo.2016.01.009
3. Spatially limited mud turbidites on the Cascadia margin: segmented earthquake ruptures? C. Goldfinger et al. 10.5194/nhess-13-2109-2013
4. Dynamic near-seafloor sediment transport in Kaikōura Canyon following a large canyon-flushing event K. Maier et al. 10.2110/jsr.2023.117
5. Geological evidence for past large earthquakes and tsunamis along the Hikurangi subduction margin, New Zealand K. Clark et al. 10.1016/j.margeo.2019.03.004
6. Estimation of successive coseismic vertical offsets using coeval sedimentary events – application to the southwestern limit of the Sea of Marmara's Central Basin (North Anatolian Fault) C. Beck et al. 10.5194/nhess-15-247-2015
7. Using pollen in turbidites for vegetation reconstructions L. McDonald et al. 10.1002/jqs.3653
8. Bimodal Recurrence Pattern of Tsunamis in South‐Central Chile: A Statistical Exploration of Paleotsunami Data P. Kempf et al. 10.1785/0220180204
9. Salt-marsh foraminiferal record of 10 large Holocene (last 7500 yr) earthquakes on a subducting plate margin, Hawkes Bay, New Zealand B. Hayward et al. 10.1130/B31295.1
10. Understanding sedimentary systems and processes of the Hikurangi Subduction Margin; from Trench to Back-Arc. Volume 1 L. Strachan et al. 10.1080/00288306.2022.2048032
11. Large earthquakes along slow converging plate margins: Calabrian Arc paleoseismicity based on the submarine turbidite record A. Polonia et al. 10.1016/j.gsf.2023.101612
12. Active Faulting, Submarine Surface Rupture, and Seismic Migration Along the Liquiñe‐Ofqui Fault System, Patagonian Andes A. Villalobos et al. 10.1029/2020JB019946
13. Deposition and preservation of tephra in marine sediments at the active Hikurangi subduction margin J. Hopkins et al. 10.1016/j.quascirev.2020.106500
14. Seafloor fault ruptures along the North Anatolia Fault in the Marmara Sea, Turkey: Link with the adjacent basin turbidite record C. McHugh et al. 10.1016/j.margeo.2014.03.005
15. Foraminiferal insights into the complexities of the turbidity currents triggered by the 2016 Kaikoura Earthquake, New Zealand B. Hayward et al. 10.1016/j.marmicro.2022.102171
16. Marine Terraces Reveal Complex Near-Shore Upper-Plate Faulting in the Northern Hikurangi Margin, New Zealand N. Litchfield et al. 10.1785/0120190208
17. An attempt to reconstruct 2700 years of seismicity using deep-sea turbidites offshore eastern Taiwan R. Lehu et al. 10.1016/j.tecto.2016.04.030
18. Sedimentary Records in the Lesser Antilles Fore‐Arc Basins Provide Evidence of Large Late Quaternary Megathrust Earthquakes C. Seibert et al. 10.1029/2023GC011152
19. On the triggers, resulting flow types and frequencies of subaqueous sediment density flows in different settings P. Talling 10.1016/j.margeo.2014.02.006
20. Untangling the complex origin of turbidite activity on the Calabrian Arc (Ionian Sea) over the last 60ka E. Köng et al. 10.1016/j.margeo.2015.12.010
21. Shear zone liquefaction in mass transport deposit emplacement: A multi-scale integration of seismic reflection and outcrop data K. Ogata et al. 10.1016/j.margeo.2014.05.001
22. Submarine paleoseismology of the northern Hikurangi subduction margin of New Zealand as deduced from Turbidite record since 16 ka H. Pouderoux et al. 10.1016/j.quascirev.2013.11.015
23. Factors affecting thickness and frequency of turbidites triggered by earthquakes in Kumburgaz Basin, Sea of Marmara N. Yakupoğlu et al. 10.1016/j.margeo.2022.106900
24. Gravity‐Driven Deposits in an Active Margin (Ionian Sea) Over the Last 330,000 Years E. Köng et al. 10.1002/2017GC006950
25. Trench floor depositional response to glacio-eustatic changes over the last 45 ka, northern Hikurangi subduction margin, New Zealand A. Woodhouse et al. 10.1080/00288306.2022.2099432
26. Marine Transform Faults and Fracture Zones: A Joint Perspective Integrating Seismicity, Fluid Flow and Life C. Hensen et al. 10.3389/feart.2019.00039
27. Understanding sedimentary systems and processes of the Hikurangi subduction margin; from Trench to Back-Arc. Volume 2 L. Strachan et al. 10.1080/00288306.2024.2358032
28. A source-to-sink perspective of the Waipaoa River margin S. Kuehl et al. 10.1016/j.earscirev.2015.10.001
29. Using foraminiferal test-size distribution and other methods to recognise Quaternary bathyal turbidites and taphonomically-modified faunas B. Hayward et al. 10.1016/j.marmicro.2019.03.008
30. Remobilization of surficial slope sediment triggered by the A.D. 2011 Mw9 Tohoku-Oki earthquake and tsunami along the Japan Trench C. McHugh et al. 10.1130/G37650.1
31. Depositional rate, grain size and magnetic mineral sulfidization in turbidite sequences, Hikurangi Margin, New Zealand A. Noda et al. 10.1080/00288306.2022.2099910
32. Foraminiferal evidence for the provenance and flow history of turbidity currents triggered by the 2016 Kaikōura Earthquake, New Zealand B. Hayward et al. 10.1080/00288306.2022.2103157
33. Turbidite paleoseismology along the active continental margin of Chile – Feasible or not? A. Bernhardt et al. 10.1016/j.quascirev.2015.04.001
34. Distribution of surficial sediments in the ocean around New Zealand/Aotearoa. Part A: continental slope and deep ocean H. Bostock et al. 10.1080/00288306.2018.1523198
35. A depositional model for seismo-turbidites in confined basins based on Ionian Sea deposits A. Polonia et al. 10.1016/j.margeo.2016.05.010
36. A revised classification and terminology for stacked and amalgamated turbidites in environments dominated by (hemi)pelagic sedimentation M. Van Daele et al. 10.1016/j.sedgeo.2017.06.007
37. Combining Conflicting Bayesian Models to Develop Paleoseismic Records: An Example from the Wasatch Fault Zone, Utah C. DuRoss et al. 10.1785/0120170302
38. Sedimentary impacts of recent moderate earthquakes from the shelves to the basin floor in the western Gulf of Corinth A. Beckers et al. 10.1016/j.margeo.2016.10.018