Blar i Bergen Open Research Archive på forfatter "Muravchik, Martin"
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Building up or out? Disparate sequence architectures along an active rift margin-Corinth rift, Greece
Gawthorpe, Rob; Andrews, Julian E.; Collier, Richard E.L.I.; Ford, Mary; Henstra, Gijs Allard; Kranis, Haralambos; Leeder, Mike R.; Muravchik, Martin; Skourtsos, Emmanuel (Peer reviewed; Journal article, 2017-12)Early Pleistocene synrift deltas developed along the southern Corinth rift margin were deposited in a single, dominantly lacustrine depocenter and were subject to the same climate-related base-level and sediment supply ... -
Deep-water sediment transport patterns and basin floortopography in early rift basins: Plio-Pleistocene syn-rift of theCorinth Rift, Greece
Muravchik, Martin; Henstra, Gijs Allard; Eliassen, Gauti; Gawthorpe, Rob; Leeder, MR; Kranis, H; Skourtsos, E; Andrews, J. (Peer reviewed; Journal article, 2019)Our current understanding on sedimentary deep‐water environments is mainly built of information obtained from tectonic settings such as passive margins and foreland basins. More observations from extensional settings are ... -
The evolution of catchment-depositional system relationships on the dip slopes of intra-rift basement highs: an example from the Frøya High, Mid-Norwegian Rifted Margin
Henstra, Gijs Allard; Cullen, Tim; Gawthorpe, Robert Leslie; Munoz Barrera, Jhon Meyer; Muravchik, Martin; Rotevatn, Atle (Journal article; Peer reviewed, 2023)Basement highs form one of many potential sediment source areas during the evolution of continental rifts and rifted margins and add to the topographic complexity typical of active rifts. Footwall basement highs acting as ... -
Tectono-sedimentary evolution of the Plio-Pleistocene Corinth rift, Greece
Gawthorpe, Rob; Leeder, Mike R.; Kranis, Haralambos; Skourtsos, E; Andrews, Julian E.; Henstra, Gijs Allard; Mack, Greg H; Muravchik, Martin; Turner, Jenni A; Stamatakis, M (Peer reviewed; Journal article, 2018-06)The onshore central Corinth rift contains a syn‐rift succession >3 km thick deposited in 5–15 km‐wide tilt blocks, all now inactive, uplifted and deeply incised. This part of the rift records upward deepening from fluviatile ...