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Member Login
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 International Geological Congress,oslo 2008
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 The influence of coals and source rocks on biological processes within the deep subsurface
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Microbial colonization of various habitable niches during alteration of oceanic crust
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Can thermodynamics help us to understand the role of life in the Earth system and its evolution?
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Phanerozoic geodynamics of the South Tian-Shan
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Microcontinents in caledonides of the Tien Shan and their geodynamic evolution in a late Precambrian - early Paleozoic
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Late Permian post-orogenic tectonics of Tianshan Belt proved by structural, geochronological, geochemical and paleomagnetic evidences
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Late Paleozoic slab break-off in the east Tianshan: Evidence from Magmatism of Balikun, Harlik
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A late Paleozoic orocline that developed in the central Asian triangle between the converging Baltica, Siberia and Tarim cratons
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New tectonic map of central Asia at 1:2.5 M scale: Trends of origination and reworking of consolidated crust
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Metallogenic and tectonic model for the Circum-North Pacific
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Deformation processes of quartz schists in the Sambagawa metamorphic belt, SW Japan and a deformation mechanism map estimated from naturally deformed rocks
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Zircon-bearing chlorite schists in the Sierra Bermeja massif (Ronda peridotites, Betic Cordilleras)
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On the active tectonics of northern Central America and the Middle America Trench: Constraints from finite element modelling
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Formation of carbonate cataclasites by fault-breccia recycling
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Plio-Quaternary tectonic evolution of the Northern Apennines thrust fronts: Seismotectonic implications
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1997-2007: 10 years of European-Mediterranean regional centroid moment tensors
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Structural evolution around the bend of the Yangsan Fault, SE Korea
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Alpine metamorphic and tectonic evolution of contact between Variscan and alpine Corsica in the Corte-Inzecca area (Corsica, France)
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(U-Th)/He dating of low T metamorphism in the Penninic sector (Ligurian Alps, Northern Italy): Inferences on deformation ages of Alpine tectonic evolution
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Fractured cobbles and outcrop-scale deformation reflect stresses associated with brittle regional detachment faulting: Titus Canyon formation, Death Valley region, California/Nevada, United States
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