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Par Collection Par Auteur- HAN HUKANG (1)
- DOORNKAMP, J. C. (1)
- LIU, Z. (1)
- MATSUMOTO, J. (1)
- PECSI, M., (Editeur scientifique) (1)
- 1985 (4)
- Physical geography (4)
- Chine ; Circulation atmosphérique ; Dynamique de l'atmosphère ; Estival ; Eté ; Front ; Front arctique Sibério-Canadien ; Front polaire Eurasien ; Front polaire Pacifique ; Géographie physique ; Précipitation ; Type de temps ; Variation spatio-temporelle (1)
- Chine ; Corrélation stratigraphique ; Datation radiocarbone ; Grotte ; Géochronologie ; Géographie physique ; Homme de Pékin ; Paléoclimatologie ; Préhistoire ; Quaternaire ; Remplissage de grotte ; Stratigraphie ; Sédimentologie ; Zhoukoudian (1)
- Chine ; Formation superficielle ; Géochimie ; Géographie physique ; Géomorphologie ; Hongrie ; Loess ; Paléontologie ; Pédologie ; Quaternaire ; Stratigraphie ; Sédimentologie (1)
- Chine ; Géographie physique ; Géomorphologie appliquée ; Géomorphologie structurale ; Méthodologie ; Néotectonique ; Recherche ; Séisme (1)
- Loess and the Quaternary: Chinese and Hungarian case studies. (1)
- Morphotectonic research in China and its application to earthquake prediction (1)
- Precipitation distribution and frontal zones over East Asia in the summer of 1979 (1)
- Sequence of sediments at Locality 1 in Zhoukoudian and correlation with loess stratigraphy in northern China and with the chronology of deep-sea cores (1)
- Morphotectonic research in China and its application to earthquake prediction
- 1985
- Sequence of sediments at Locality 1 in Zhoukoudian and correlation with loess stratigraphy in northern China and with the chronology of deep-sea cores
- , permitted correlation with events both within China and farther afield, and placed the sequence in the global framework of late Cenozoic climatic change. The cave deposits can be divided into 17 layers which are correlated with the great loess sequences (L9
- -L4) in China and with deep-sea-core oxygen-isotope stages 16-6. The 14th layer upward (730,000-230,000 yr B.P.) represents at least four glacial cycles.
- 1985
- Central China and southern coast of Japan during the Bain season, shifts north from mid-July to mid-August. It brings much rain over North China Plain, Primosky and Sakhalin during mid-summer. While, the locations of other frontal zones change little
- 1985
- and geochemistry are summarized to promote their application in the related sciences. Correlations are drawn between loesses in China and in Hungary. (DLO).
- 1985