How and why small volcanic ocean islands collapse and move vertically up and down. [PDF]
Marques FO +4 more
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Precise dating of large flank collapses by single-grain 40Ar/39Ar on pyroclastic deposits from the example of Flores Island (Azores). [PDF]
Hildenbrand A +4 more
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Landslide topology uncovers failure movements. [PDF]
Bhuyan K +6 more
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Impact of Cable Structure on Distributed Fiber Optic Sensing
Cappelli G +12 more
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3-D intrinsic attenuation tomography using ambient seismic noise applied to La Palma Island (Canary Islands). [PDF]
Cabrera-Pérez I +9 more
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Physical experiments of waves generated by submerged steam eruptions with applications to volcanic tsunamis. [PDF]
Shen Y +4 more
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Report and preliminary results of R/V POSEIDON Cruise POS472, NORGEotech, Geotechnical in situ investigation of slope stability in Norway, Trondheim (Norway) - Tromsø (Norway), 27.07.2014 - 12.08.2014 [PDF]
Baeten, N. +10 more
core
Integrating machine learning and geomorphic indices to assess tectonic geomorphology in the Karoun River Basin, Zagros, SW Iran. [PDF]
Khodabakhshnezhad A +5 more
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Numerical investigation of production performance of challenging gas hydrates from deposits with artificial fractures and impermeable barriers. [PDF]
Nie S +7 more
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Landslides are common on inclined areas of the seafloor, particularly in environments where weak geologic materials such as rapidly deposited, fine‐grained sediment or fractured rock are subjected to strong environmental stresses such as earthquakes, large storm waves, and high internal pore pressures.
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