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. 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. 10.1002/2017JB014181
3. Fluid and mass transfer at subduction interfaces—The field metamorphic record G. Bebout & S. Penniston-Dorland 10.1016/j.lithos.2015.10.007
4. Modeling Trench Sediment‐Controlled Flow in Subduction Channels: Implications for the Topographic Evolution of the Central Andean Fore Arc N. Cosentino et al. 10.1029/2018JB016109
5. The Franciscan Complex (California, USA) – The model case for return-flow in a subduction channel put to the test A. Krohe 10.1016/j.gr.2017.02.003
6. Material transfer and subduction channel segmentation at erosive continental margins: Insights from scaled analogue experiments F. Albert et al. 10.1016/j.tecto.2018.10.019
7. Forced Return Flow Deep in the Subduction Channel, Syros, Greece U. Ring et al. 10.1029/2019TC005768
8. 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 10.1016/j.earscirev.2020.103356
9. The subduction plate interface: rock record and mechanical coupling (from long to short timescales) P. Agard et al. 10.1016/j.lithos.2018.09.029
10. 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. 10.1016/j.gca.2015.04.024
11. Polyphase brittle and ductile deformation of Late Jurassic ophiolitic basalt-argillite matrix mélange and stratigraphic overlap sequence, northwestern Washington State D. Katopody & J. Oldow 10.1016/j.gr.2019.01.005