CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER

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CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER

郭鹏飞, 边纯玉

文章导航 > Chinese Geographical Science > 1993 > 3(2): 163-172

郭鹏飞, 边纯玉. CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER[J]. 中国地理科学, 1993, 3(2): 163-172.

引用本文:

郭鹏飞, 边纯玉. CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER[J]. 中国地理科学, 1993, 3(2): 163-172.

Guo Pengfei, Bian Chunyu. CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER[J]. Chinese Geographical Science, 1993, 3(2): 163-172.

Citation:

Guo Pengfei, Bian Chunyu. CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER[J]. Chinese Geographical Science, 1993, 3(2): 163-172.

CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER

郭鹏飞¹,
边纯玉²

1.
Lanzhou Hydrogeological and Engineering Geologic Centre, Ministry of Geology and Minerals, Lanzhou 730000, PRC;
2.
906 Hydrogeological and Engineering Geologic Team, Ministry of Geology and Minerals, Xining 810000, PRC

CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER

Guo Pengfei¹,
Bian Chunyu²

1.
Lanzhou Hydrogeological and Engineering Geologic Centre, Ministry of Geology and Minerals, Lanzhou 730000, PRC;
2.
906 Hydrogeological and Engineering Geologic Team, Ministry of Geology and Minerals, Xining 810000, PRC

摘要: There widely occur stretches of permafrost at more than 3,800-4,200 meters above sea level in the source area of the Huanghe (Yellow) River. The periglacial geomorphology develops quite well, including frozen disintegration geomorphology, freezing and thawing geomorphology in cold environments, periglacial dune, buried ices and fossil periglacial phenomena. In light of the relation between stratigraphy and periglacial phenomena, three periglacial periods can be divided, which are the Middle Pleistocene periglacial period, the Late Pleistocene periglacial period and modern periglacial period.
- source area of the Huanghe River /
- periglacial geomorphology /
- periglacial period
Abstract: There widely occur stretches of permafrost at more than 3,800-4,200 meters above sea level in the source area of the Huanghe (Yellow) River. The periglacial geomorphology develops quite well, including frozen disintegration geomorphology, freezing and thawing geomorphology in cold environments, periglacial dune, buried ices and fossil periglacial phenomena. In light of the relation between stratigraphy and periglacial phenomena, three periglacial periods can be divided, which are the Middle Pleistocene periglacial period, the Late Pleistocene periglacial period and modern periglacial period.
- source area of the Huanghe River /
- periglacial geomorphology /
- periglacial period

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CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER

郭鹏飞¹,
边纯玉²

1. Lanzhou Hydrogeological and Engineering Geologic Centre, Ministry of Geology and Minerals, Lanzhou 730000, PRC;

2. 906 Hydrogeological and Engineering Geologic Team, Ministry of Geology and Minerals, Xining 810000, PRC

刊出日期: 1993-06-20

关键词:

source area of the Huanghe River /

periglacial geomorphology /

periglacial period

摘要: There widely occur stretches of permafrost at more than 3,800-4,200 meters above sea level in the source area of the Huanghe (Yellow) River. The periglacial geomorphology develops quite well, including frozen disintegration geomorphology, freezing and thawing geomorphology in cold environments, periglacial dune, buried ices and fossil periglacial phenomena. In light of the relation between stratigraphy and periglacial phenomena, three periglacial periods can be divided, which are the Middle Pleistocene periglacial period, the Late Pleistocene periglacial period and modern periglacial period.

English Abstract

郭鹏飞, 边纯玉. CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER[J]. 中国地理科学, 1993, 3(2): 163-172.

引用本文:

郭鹏飞, 边纯玉. CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER[J]. 中国地理科学, 1993, 3(2): 163-172.

Guo Pengfei, Bian Chunyu. CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER[J]. Chinese Geographical Science, 1993, 3(2): 163-172.

Citation:

Guo Pengfei, Bian Chunyu. CHARACTERISTICS OF PERIGLACIAL GEOMORPHOLOGY IN THE SOURCE AREA OF THE HUANGHE RIVER[J]. Chinese Geographical Science, 1993, 3(2): 163-172.

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