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  •  International Geological Congress,oslo 2008
      First evidence of Cordevolian (lower Carnian) radiolarians at the base of the Upper Antalya Nappes, Turkey
      Jurassic and Cretaceous radiolarian biostratigraphy of the Pichakun and Hawasina basins
      Striped radiolarian chert: evidence for superimposed cyclicity in the Earth System
      Life in the Precambrian Sea: A window to global biotic events from India
      The complexities of accessory minerals in the Catoca kimberlite as revealed by a LA-ICP-MS investigation
      Physico-chemical conditions of formation of mantle-derived diamond and its syngenetic inclusions by HPHT experimental evidence
      Experimental model for alkalic chloride-rich diamond-forming liquids in the upper mantle
      The electrical anisotropy of the continental lithosphere: Methods of analysis and results for southern Africa
      On upper mantle heterogeneity and anisotropy as mapped by inversion of global surface wave data
      Fine scale heterogeneity in the earth’s crust and mantle
      Exploring the role of subducted crust and residue in explaining mantle heterogeneity using numerical simulations
      Petrographic and geochemical comparison between Early to Middle Cambrian and Uppermost Cambrian-Lower Ordovician quartz-rich sandstones in NW Argentina
      Detrital zircon geochronology of Neoproterozoic successions reveals the Mesoproterozoic to Cambrian evolution of the Raío de la Plata Craton
      A-type rift-related granite and the lower cryogenian age for the beginning of the Brusque Belt Basin, Dom Feliciano Belt, Southern Brazil
      Huge vertical displacement during post-collisional escape tectonic (Brasiliano Orogeny) of the Ribeira Belt, Sمo Paulo, Brazil
      From the canadian shield to north american subcontinent
      Seismic images of the Svecofennian accretionary orogen
      Timing of syn-tectonic granites in the early Paleozoic Wuyishan fold belt (South China) with tectonic implications
      Late darriwilian — early Caradocian felsic volcanism and coeval migmatizaton in a peri-Gondwanan island arc complex, newfoundland appalachians
      How does an accreted island arc end up sandwiched between quartz-rich continental margin turbidites? lessons from the lachlan orogen of southeastern Australia
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