Blar i Bergen Open Research Archive på forfatter "Mazzini, Adriano"

Viser treff 1-3 av 3

    • A climatic trigger for the giant Troll pockmark field in the northern North Sea 

      Mazzini, Adriano; Svensen, Henrik; Forsberg, Carl Fredrik; Linge, Henriette; Lauritzen, Stein-Erik; Haflidason, Haflidi; Hammer, Øyvind; Planke, Sverre; Tjelta, Tor-Inge (Peer reviewed; Journal article, 2017-04)
      Pockmarks are seafloor craters usually formed during methane release on continental margins. However, the mechanisms behind their formation and dynamics remain elusive. Here we report detailed investigations on one of the ...

    • Sanctuary for vulnerable Arctic species at the Borealis Mud Volcano 

      Panieri, Giuliana; Argentino, Claudio; Savini, Alessandra; Ferré, Benedicte; Hemmateenejad, Fereshteh; Eilertsen, Mari Heggernes; Mattingsdal, Rune; Ramalho, Sofia P.; Eidvin, Tor; Youngs, Sarah; Colson, Beckett Casper; Michel, Anna Pauline Miranda; Kapit, Jason Alexander; Swanborn, Denise; Rogers, Alex D.; Barrenechea Angeles, Inés; Polteau, Stephane; Kalenitchenko, Dimitri Stanislas Desire; Bünz, Stefan; Mazzini, Adriano (Journal article; Peer reviewed, 2025)
      Borealis is a recently discovered submerged mud volcano in the Polar North Atlantic, differing from the numerous methane seepages previously identified in the region. Here we show in situ observations from a remotely ...

    • Upper cretaceous-paleogene stratigraphy and development of the Mímir High, Vøring transform margin, Norwegian Sea 

      Polteau, Stephane; Planke, Sverre; Zastrozhnov, Dmitrii; Abdelmalak, Mohamed Mansour; Lebedeva-Ivanova, Nina; Eckhoff Planke, Ellen; Svensen, Henrik; Mazzini, Adriano; Gernigon, Laurent; Myklebust, Reidun; Kjølhamar, Bent; Pedersen, Rolf B.; Sandstå, Nils Rune; Bünz, Stefan (Journal article; Peer reviewed, 2020)
      Transform margins represent strike-slip type of plate boundaries that form during continental breakup and initial ocean opening. They are often characterized by margin-parallel highs with exposed pre- and syn-rift sequences. ...