THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION

文启忠; 施雅风

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THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION

文启忠, 施雅风

文章导航 > Chinese Geographical Science > 1993 > 3(2): 147-158

文启忠, 施雅风. THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION[J]. 中国地理科学, 1993, 3(2): 147-158.

引用本文:

文启忠, 施雅风. THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION[J]. 中国地理科学, 1993, 3(2): 147-158.

Wen Qizhong, Shi Yafeng. THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION[J]. Chinese Geographical Science, 1993, 3(2): 147-158.

Citation:

Wen Qizhong, Shi Yafeng. THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION[J]. Chinese Geographical Science, 1993, 3(2): 147-158.

THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION

文启忠¹,
施雅风²

1.
Guangzhou Branch of Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PRC;
2.
Lanzhou Institute of Glaciology and Geocryology, Chinese A cademy of Sciences, Lanzhou 710000, PRC

THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION

Wen Qizhong¹,
Shi Yafeng²

1.
Guangzhou Branch of Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PRC;
2.
Lanzhou Institute of Glaciology and Geocryology, Chinese A cademy of Sciences, Lanzhou 710000, PRC

摘要: This paper describes the paleoclimatic changesoccurring in the Chaiwopu Basin since 730,000 yr.B.P., together with theformation and evolution of Chaiwopu Lake based on the chronology and characteristics of a core drilled in the basin. Analysis of the drilling core provides information on the climate and environment of the area. It would appear that the paleoclimatic changes that occurred in the basin during the Pleistocene was controlled by the relationship between the sun and the earth and by Long-term (10,000 yr.) climatic cycles. The climate tended to cold-dry during the glacial period (ice age) and warm-moist during the interglacial. Following the warm period of the Holocene, short-term (1,000 yr.) climatic cycles occurred in cool-moist periods, similar to the "Little Ice Age", alternated with warm-dry periods.
- paleoclimate /
- environment changes /
- Quaternary /
- Xinjiang
Abstract: This paper describes the paleoclimatic changesoccurring in the Chaiwopu Basin since 730,000 yr.B.P., together with theformation and evolution of Chaiwopu Lake based on the chronology and characteristics of a core drilled in the basin. Analysis of the drilling core provides information on the climate and environment of the area. It would appear that the paleoclimatic changes that occurred in the basin during the Pleistocene was controlled by the relationship between the sun and the earth and by Long-term (10,000 yr.) climatic cycles. The climate tended to cold-dry during the glacial period (ice age) and warm-moist during the interglacial. Following the warm period of the Holocene, short-term (1,000 yr.) climatic cycles occurred in cool-moist periods, similar to the "Little Ice Age", alternated with warm-dry periods.
- paleoclimate /
- environment changes /
- Quaternary /
- Xinjiang

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THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION

文启忠¹,
施雅风²

1. Guangzhou Branch of Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PRC;

2. Lanzhou Institute of Glaciology and Geocryology, Chinese A cademy of Sciences, Lanzhou 710000, PRC

刊出日期: 1993-06-20

关键词:

paleoclimate /

environment changes /

Quaternary /

Xinjiang

摘要: This paper describes the paleoclimatic changesoccurring in the Chaiwopu Basin since 730,000 yr.B.P., together with theformation and evolution of Chaiwopu Lake based on the chronology and characteristics of a core drilled in the basin. Analysis of the drilling core provides information on the climate and environment of the area. It would appear that the paleoclimatic changes that occurred in the basin during the Pleistocene was controlled by the relationship between the sun and the earth and by Long-term (10,000 yr.) climatic cycles. The climate tended to cold-dry during the glacial period (ice age) and warm-moist during the interglacial. Following the warm period of the Holocene, short-term (1,000 yr.) climatic cycles occurred in cool-moist periods, similar to the "Little Ice Age", alternated with warm-dry periods.

English Abstract

文启忠, 施雅风. THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION[J]. 中国地理科学, 1993, 3(2): 147-158.

引用本文:

文启忠, 施雅风. THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION[J]. 中国地理科学, 1993, 3(2): 147-158.

Wen Qizhong, Shi Yafeng. THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION[J]. Chinese Geographical Science, 1993, 3(2): 147-158.

Citation:

Wen Qizhong, Shi Yafeng. THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION[J]. Chinese Geographical Science, 1993, 3(2): 147-158.

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THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION

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THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION

1. Guangzhou Branch of Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PRC; 2. Lanzhou Institute of Glaciology and Geocryology, Chinese A cademy of Sciences, Lanzhou 710000, PRC

English Abstract

THE QUATERNARY CLIMO-ENVIRONMENT CHANGES IN CHAIWQPU BASIN OF XINJIANG REGION

1. Guangzhou Branch of Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PRC; 2. Lanzhou Institute of Glaciology and Geocryology, Chinese A cademy of Sciences, Lanzhou 710000, PRC

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目录

1. Guangzhou Branch of Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PRC;

2. Lanzhou Institute of Glaciology and Geocryology, Chinese A cademy of Sciences, Lanzhou 710000, PRC

1. Guangzhou Branch of Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, PRC;

2. Lanzhou Institute of Glaciology and Geocryology, Chinese A cademy of Sciences, Lanzhou 710000, PRC