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     International Geological Congress,oslo 2008
      Numerical investigations of particle suspensions
      Geometry and kinematics of thrust sheets in the High Zagros zone at Bakhtyari area, Iran
      Comparing structural styles in the Apennines fold-and-thrust belt: constraints from thermal, thermochronometric and structural data
      Structure and evolution of a near-classic thrust and fold belt: The case of the Umbria-Marche Apennines (Central Italy)
      Pulsed south-westerly migration of the Zagros deformation front during the Miocene-Recent: Seismic evidence from the Persian Gulf
      Thrust-zone localization – the importance of distributed strains and buckling
      Are epicontinental rift sedimentary basins fertile tectonic environments for gold? reflections on the north-central Nevada gold province
      Synchronous vertical and horizontal tectonism at the late stages of Archean cratonization is an important process for gold mineralization
      The source of the world’s largest accumulation of gold
      Temporal-spatial relationships between tectonism, magmatism, and orogenic gold deposit formation in the north American Cordillera
      Late-stage mineral formation of Noril’sk ore field and its genetic relations
      Geobotanical and biogeochemical nickel ore prospecting in Northern Finland
      Re-Os and Sm-Nd isotopes of magmatic Ni-Cu sulfides from a Mesoproterozoic convergent plate margin
      Nickel sulfide deposition during 1.88 Ga - examples from the orogenic Kotalahti Nickel Belt compared with the Thompson and Cape Smith Nickel Belts
      Tectonomagmatic settings of magmatic Ni-Cu-(PGE) deposits
      Markasheh sediment-hosted stratiform Cu mineralization in the Ravar region, Central Iran
      Sulfur isotope values in the Talvivaara Ni-Cu-Zn and Outokumpu Cu-Co-Zn-Ni-Ag-Au deposits: Evidence for a genetic connection between black shale and sulfide ore
      Chahmir deposit: A sedimentary-exhalative Zn-Pb deposit in Bafq basin, Central Iran
      Fossile Fe-Mn-oxide chimneys?
      Metalliferous organic-rich black shales: Are exhalative hydrothermal processes fundamental to their genesis?
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