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  •  International Geological Congress,oslo 2008
      Scotland’s fjord landsystem
      Holocene Rapid Climate Change: Pervasive millennial-scale climate variability in the NE Atlantic
      The medieval warm period and the Little Ice Age in marine sediments from Maxwell Bay, King George Island, West Antarctic Peninsula
      The exceptionally thick, expanded sedimentary fill of the Crane Glacier Trough: a new-born fjord following the collapse of Larsen B Ice Shelf, Antarctica
      Regional change and local input: The significance of local events for the interpretation of environmental change from fjord sediments
      The eclogite, blueschists in central Qiangtang, Tibet, China: The record of Triassic subduction belt
      Petrography and evolution of Somdo eclogites, Qinghai-Tibetan plateau: Another possible continental plate subduction belt
      The intrusive nature of quartzites of the Makbal complex, Tien-Shan, Kyrgyzstan
      Progresses, controversies and challenges of studies on South Altyn Tagh-North Qaidam HP/UHP metamorphic belt, northwestern China
      High- to ultra-high pressure partial melting in orogenic belts: Implications for the formation of felsic granulites from the Bohemian Massif
      Structural geometry of an exhumed UHP terrane and its implication for continental collisional processes: A case study from Yangkou Bay, Sulu orogen
      Passive Continental Margin Fold and Thrust Belts
      Deep-water fold-and-thrust belts in the Amazon deep-sea fan
      Migration of fault activity in the southwestern kanto plain, central Japan
      Lacustrine sedimentary records as complements to trench paleoseismic investigations: An example along the Boconó fault, north-western Venezuela
      Anomalous concentration of rock avalanche deposits at the eastern slope of the Argentinean Andes between 36°-38°S
      Towards a catalogue of earthquake environmental effects
      The role of active (capable) faults in paleoseismicity
      Deposits of thermohaline currents on slopes in the North East Atlantic Ocean — implications for climate change
      Hatton drift textural evidence of late quaternary changes of deep western boundary current
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