11 citations as recorded by crossref.

1. Crystallographic preferred orientations of exhumed subduction channel rocks from the Eclogite Zone of the Tauern Window (Eastern Alps, Austria), and implications on rock elastic anisotropies at great depths R. Keppler et al. https://doi.org/10.1016/j.tecto.2015.02.011
2. Textures of eclogites and blueschists from Syros island, Greece: Inferences for elastic anisotropy of subducted oceanic crust R. Keppler et al. https://doi.org/10.1002/2017JB014181
3. Modeling Trench Sediment‐Controlled Flow in Subduction Channels: Implications for the Topographic Evolution of the Central Andean Fore Arc N. Cosentino et al. https://doi.org/10.1029/2018JB016109
4. The Franciscan Complex (California, USA) – The model case for return-flow in a subduction channel put to the test A. Krohe https://doi.org/10.1016/j.gr.2017.02.003
5. Material transfer and subduction channel segmentation at erosive continental margins: Insights from scaled analogue experiments F. Albert et al. https://doi.org/10.1016/j.tecto.2018.10.019
6. Zoning of eclogitic garnet cores – a key pattern demonstrating the dominance of tectonic erosion as part of the burial process of worldwide occurring eclogites H. Massonne & B. Li https://doi.org/10.1016/j.earscirev.2020.103356
7. Polyphase brittle and ductile deformation of Late Jurassic ophiolitic basalt-argillite matrix mélange and stratigraphic overlap sequence, northwestern Washington State D. Katopody & J. Oldow https://doi.org/10.1016/j.gr.2019.01.005
8. Fluid and mass transfer at subduction interfaces—The field metamorphic record G. Bebout & S. Penniston-Dorland https://doi.org/10.1016/j.lithos.2015.10.007
9. Forced Return Flow Deep in the Subduction Channel, Syros, Greece U. Ring et al. https://doi.org/10.1029/2019TC005768
10. The subduction plate interface: rock record and mechanical coupling (from long to short timescales) P. Agard et al. https://doi.org/10.1016/j.lithos.2018.09.029
11. B, Sr and Pb isotope geochemistry of high-pressure Alpine metaperidotites monitors fluid-mediated element recycling during serpentinite dehydration in subduction mélange (Cima di Gagnone, Swiss Central Alps) E. Cannaò et al. https://doi.org/10.1016/j.gca.2015.04.024