Results 121 to 130 of about 530 (149)
Five-Year Persistence of Vedolizumab in Crohn's Disease: Results from a Real-World Cohort. [PDF]
Harb M, Muls V, Hoyois A, Aoun J.
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Experimental vibration dataset collected of a beam reinforced with masses under different health conditions. [PDF]
de Sousa AASR, Machado MR.
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Improvement of Light Output of MAPbBr3 Single Crystal for Ultrafast and Bright Cryogenic Scintillator. [PDF]
Mahato S +9 more
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"Polonez grany dźwiękiem słów" : o muzyczności słowa w dramatach Wyspiańskiego
openaire +1 more source
The middle to late Oligocene Polonez Cove Formation, exposed on south‐eastern King George Island, South Shetland Islands, provides rare evidence of mid‐Cenozoic West Antarctic cryosphere evolution. A revised lithostratigraphy and facies analysis and a review of the palaeoenvironmental significance of the formation are presented here.
John Smellie
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Invertebrates From the Low Head Member (Polonez Cove Formation, Oligocene) at Vauréal Peak, King George Island, West Antarctica [PDF]
AbstractEight taxa of marine invertebrates, including two new bivalve species, are described from the Low Head Member of the Polonez Cove Formation (latest early Oligocene) cropping out in the Vauréal Peak area, King George Island, West Antarctica. The fossil assemblage includes representatives of Brachiopoda (generaNeothyrissp.
Antonio Carlos Rocha-Campos
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Shell Beds From the Low Head Member (Polonez Cove Formation, Early Oligocene) at King George Island, West Antarctica: New Insights on Facies Analysis, Taphonomy and Environmental Significance [PDF]
AbstractShell bed levels in the Low Head Member of the early Oligocene Polonez Cove Formation at King George Island, West Antarctica, are re-interpreted based on sedimentological and taphonomic data. The highly fossiliferous Polonez Cove Formation is characterized by basal coastal marine sandstones, overlain by conglomerates and breccias deposited in ...
Fernanda Quaglio +2 more
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Journal of the Geological Society, 2021
Zircon grains from nine erratic pebbles of granite, granodiorite–tonalite and quartzite from the Polonez Cove Formation (southern King George Island) were studied for their U–Pb isotope ages and provenance. The calculated concordia ages of the studied pebbles are 108.79 ± 0.89, 119.7 ± 2.2, 178.6 ± 2.8, 180.7 ± 1.9, 207.4 ± 3.1, 231.1 ± 1.9, 1087.5 ± 4
Magdalena Pańczyk +2 more
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Zircon grains from nine erratic pebbles of granite, granodiorite–tonalite and quartzite from the Polonez Cove Formation (southern King George Island) were studied for their U–Pb isotope ages and provenance. The calculated concordia ages of the studied pebbles are 108.79 ± 0.89, 119.7 ± 2.2, 178.6 ± 2.8, 180.7 ± 1.9, 207.4 ± 3.1, 231.1 ± 1.9, 1087.5 ± 4
Magdalena Pańczyk +2 more
exaly +3 more sources

