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Cui, ZJ
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Subglacial deformation: evidence from microfabric studies of particles and voids...
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Longitudinal variations in cross-section morphology along a glacial valley: a ca...
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Origin of a bouldery diamicton, Kunlun pass, Qinghai-Xizang plateau, People's Re...
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GELIFLUCTION IN THE ALPINE PERIGLACIAL ENVIRONMENT OF THE TIANSHAN MOUNTAINS, CH...
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Relationship between the distribution of periglacial landforms and glaciation hi...
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Thermal-contraction-crack networks as evidence for late-pleistocene permafrost i...
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The stratified slope deposits at Kunlunshan Pass, Tibet Plateau, China
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CHARACTERISTICS OF THE PERMAFROST STRUCTURE ON THE FILDES PENINSULA, KING GEORGE...
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Thermal-contraction-crack networks as evidence for late-pleistocene permafrost i...
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Discovery of ice wedge and sand-wedge networks in Inner Mongolia and Shanxi Prov...
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Thermal contraction crack networks as evidence for Late-Pleistocene permafrost i...
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Discovery of a large area of ice-wedge networks in Ordos: Implications for the s...
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Discovery of a large area of ice-wedge networks in Ordos: Implications for the s...
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Related Subjects
permafrost
AGE
FEATURES
ICE
Last Glaciation
Megathermal
SAND VEINS
WEDGES
false ice wedge
inner Mongolia
last glacial maximum
palaeoclimate
sand wedge
sand wedges
1989 EXPLANATION
ACTIVE LAYER
ANIYA 1988
Antarctica
BED CONDITIONS
DRUMLINS
EROSION
FABRICS
GELIFLUCTION
GEOELECTRICAL PROSPECTINGS
GLACIER
GRAIN-SIZE DISTRIBUTIONS
GRANULARITY PARAMETER
Geography
Geology
HIRANO
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