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《Journal of Glaciology and Geocryology》 1988-04
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Periglacial Phenomena and Their Age in the Valleys of Eastern Mountainous Area of Heilongjiang Province

Chen Shuhan (Shenyang Institute oj Geology and Mineral Resources )  
In the valleys of the eastern mountainous area of Heilongjiang province from Mohe in the north to Dongning in the south, the Quaternary strata of first-order bench are mainly fluvial origin. The fossil periglacial phenomena are widely and well developed in over twenty sections of quaternary and exposed in Xinlonggou district of Huma county, Wudaogou district of Aihei county and Tuanjiegou district of Jiaying county. A group of samples have been collected for 14C dating,thermoluminescence, paleomagnetic and palynologic determinations. The corresponding test results from the samples are obtained. In the Daqing section, which is in Tuanjiegou district by the southern limit of permafrost and 8 m in thickness, four freezing-melting involution layers were recognized. Based on the isptopic datings and paleomagnetic data, the ages of periglacial action may be separated into four stages: the Middle Tuanjiegou periglacial stage (47 400 ± 2800-22 000± 250 B.P.); the early Late Tuanjiegou periglacial stage (14 800 ± 740-13 000 B.P.); the late Late Tuanjiegou periglacial stage (11 370± 110-10 000 B.P.) and the Daqing periglacial stage (about 6500 B. P.).
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Chinese Journal Full-text Database 4 Hits
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2 Sun Jianzhong (Xian Geology College);Preliminary Reconstruction of the Temperature Curve of the Last Major Climatic Cycle in North China[J];Journal of Glaciology and Geocryology;1985-04
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