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Junling Pei

Dados Biográficos

ID6375269
NOMEJunling Pei
PRENOMESJunling
SOBRENOMEPei
ASSINATURAPEI J
AFILIAÇÕESChinese Academy of Geological Sciences
ORCID0000-0003-4046-3432
VERIFICADOSim
TOTAL DE OBRAS1
TOTAL DE CITAÇÕES1
TOTAL COMO AUTOR1
TOTAL COMO EDITOR0
PRIMEIRO ANO DE PUBLICAÇÃO2015
ANO MAIS RECENTE DE PUBLICAÇÃO2015
ÍNDICE H1
  • High-resolution magnetic and palynological records of the last deglaciation and Holocene from Lake Xiarinur in the Hunshandake Sandy Land, Inner Mongolia

    Open Access•Ling Tang, Xisheng Wang et al.•ARTICLE•The Holocene•2015•Citada por: 1•Referências: 12

    High-resolution mineral magnetic and pollen records from overlapping piston cores from Lake Xiarinur (42°37′N, 115°28′E) document detailed changes in environment and vegetation since the last deglaciation in the Hunshandake Sandy Land, Inner Mongolia. The formation of Lake Xiarinur commenced during the Bølling–Allerød warming, as reflected by an abrupt shift in sedimentary facies from eolian sands to lacustrine sediments at a core depth of 3.5 m …

  • High-resolution magnetic and palynological records of the last deglaciation and Holocene from Lake Xiarinur in the Hunshandake Sandy Land, Inner Mongolia

    Open Access•Ling Tang, Xisheng Wang et al.•ARTICLE•The Holocene•2015•Citada por: 1•Referências: 12

    High-resolution mineral magnetic and pollen records from overlapping piston cores from Lake Xiarinur (42°37′N, 115°28′E) document detailed changes in environment and vegetation since the last deglaciation in the Hunshandake Sandy Land, Inner Mongolia. The formation of Lake Xiarinur commenced during the Bølling–Allerød warming, as reflected by an abrupt shift in sedimentary facies from eolian sands to lacustrine sediments at a core depth of 3.5 m …

  • High-resolution magnetic and palynological records of the last deglaciation and Holocene from Lake Xiarinur in the Hunshandake Sandy Land, Inner Mongolia

    Open Access•Ling Tang, Xisheng Wang et al.•ARTICLE•The Holocene•2015•Citada por: 1•Referências: 12

    High-resolution mineral magnetic and pollen records from overlapping piston cores from Lake Xiarinur (42°37′N, 115°28′E) document detailed changes in environment and vegetation since the last deglaciation in the Hunshandake Sandy Land, Inner Mongolia. The formation of Lake Xiarinur commenced during the Bølling–Allerød warming, as reflected by an abrupt shift in sedimentary facies from eolian sands to lacustrine sediments at a core depth of 3.5 m …

Allerød oscillation (1 obras) · Deglaciation (1 obras) · Ecology (1 obras) · Geography (1 obras) · Geology (1 obras) · Geology and Paleoclimatology Research (1 obras) · Geomagnetism and Paleomagnetism Studies (1 obras) · Holocene (1 obras) · Oceanography (1 obras) · Paleontology (1 obras)

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