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East Antarctic sources of extensive Lower–Middle Ordovician turbidites in the La...
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A cryptic Gondwana-forming orogen located in Antarctica
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Dynamic recrystallization associated with gas composition changes in basal ice f...
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Evidence of bed deformation beneath the Wright Lower Glacier, South Victoria Lan...
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Dissolved organic phosphorus uptake by marine phytoplankton is enhanced by the p...
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Ice crystal properties of amber ice and strain enhancement at the base of cold A...
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Structure and strength of basal ice and substrate of a dry-based glacier: Eviden...
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Ice composition evidence for the formation of basal ice from lake water beneath...
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Equifinality of basal ice facies from an Antarctic cold-based glacier
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Ice formation in an Antarctic glacier-dammed lake and implications for glacier-l...
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Marine ice recycling at the southern McMurdo Ice Shelf, Antarctica
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Detrital zircon and igneous protolith ages of high-grade metamorphic rocks in th...
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Chemical characteristics and origin of clear basal ice facies in dry-based glaci...
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Ice crystal properties of amber ice and strain enhancement at the base of cold A...
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Seasonal sediment fluxes forcing supraglacial melting on the Wright Lower Glacie...
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Anatomy of the Kuunga Orogen in East Antarctica
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Deformation of meteoric and marine ice at the southern McMurdo Ice Shelf, Antarc...
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Superimposed tectonic events at 2450 Ma, 2100 Ma, 900 Ma and 500 Ma in the North...
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Two stages of zircon and monazite growth in anatectic leucogneiss: SHRIMP constr...
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Trapping of aeolian sediments and build‐up of the ice cover of a dry‐based Antar...
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Antarctica
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GE1-350
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