Biblioteca Digital

104 resultados para Central Banks

Pollen record from red clay sequence in the central Loess Plateau between 8.10 and 2.60 Ma

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Red clay sediment in the central Chinese Loess Plateau and its implication for the uplift of the Tibetan Plateau

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Late Pliocene-Pleistocene changes in mass accumulation rates of eolian deposits on the central Chinese Loess Plateau

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Tree-ring-based reconstruction of the April to September mean temperature since 1826 AD for north-central Shaanxi Province, China,

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Reconstructing in-situ vegetation dynamics using carbon isotopic composition of biopolymeric residues in the central Chinese Loess Plateau

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Statistical and process-based modeling analyses of tree growth response to climate in semi-arid area of north central China: A case study of Pinus tabulaeformis

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Tracing the provenance of fine-grained dust deposited on the central Chinese Loess Plateau

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Rare earth elements and yttrium in a stalagmite from Central China and potential paleoclimatic implications

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Temperature variations recorded in Pinus tabulaeformis tree rings from the southern and northern slopes of the central Qinling Mountains, central China

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Lake surface fluctuations since the late glaciation at Lake Daihai, North central China: A direct indicator of hydrological process response to East Asian monsoon climate

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Seasonal variation in nature and chemical compositions of spring water in Cuihua Mountain, Shaanxi Province, central China

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Early to mid-Pleistocene ostracod δ18O and δ13C in the central Tibetan Plateau:Implication for Indian monsoon change

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Loess magnetic properties in the Ili basin, Central Asia and their correlation with the Chinese Loess Plateau.

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Comment on “Mudflat/distal fan and shallow lake sedimentation (upper Vallesian–Turolian) in the Tianshui Basin, Central China: Evidence against the late Miocene eolian loess” by A.M. Alonso-Zarza, Z. Zhao, C.H. Song, J.J. Li, J. Zhang, A. Martín-Pérez, R. Martín-García, X.X. Wang, Y. Zhang and M.H. Zhang [Sedimentary Geology 222 (2009) 42–51]

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Large variations of oxygen isotopes in precipitation over south-central Tibet during Marine Isotope Stage 5

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