LI Yuyuan,SHI Hui.The Impact of Neotectonics on the Environmental Evolution and Soil Erosion of Loess Plateau[J].Research of Soil and Water Conservation,2001,8(01):123-129.
新构造运动对黄土高原环境变迁的影响
- Title:
- The Impact of Neotectonics on the Environmental Evolution and Soil Erosion of Loess Plateau
- Keywords:
- Neotectonics; Loess Plateau; landform evolution; climate vicissitude; environmental evolution
- 分类号:
- X144
- 摘要:
- 新构造运动是黄土高原区域环境变迁的主导性因素。25Ma以来青藏高原的阶段性强烈隆升，导致了东亚季风气候的形成和加强，黄土高原乃至整个西北地区气候向干旱化趋势演化。黄土高原及其周边地区的阶段性隆升或沉降与气候演化的共同作用，导致了黄土堆积沉积的跳跃式阶段性扩展。黄土高原的地貌演化可以黄河水系的诞生为界限(1.67～1.43MaB.P.)划分为二个阶段：古湖泊低地阶段和高原河流阶段。
- Abstract:
- Neotectonics was the dominant factor of the environmental evolution of Loess Plateau. Since 2.5 MaB.P., because of the periodical uplift of Qinghai Xizang Plateau, the monsoon climate was developed and gradually strengthened, and correspondingly the climate of Loess Plateau and even the whole west northern region of China have correspondingly been tending to become more and more arid. Sinc 2.5 MaB.P., together with the climatic evolution, the periodical uplift or subsidence of Loess Plateau and its around area induced the bouncing and periodical enlargement of the deposition of loess. The landform of Loess Plateau may be divided into two stages: ancient lake low lying land stages and plateau river stage.
参考文献/References:
[1] 孙鸿烈,郑度.青藏高原形成演化与发展[M].广州:广东科技出版社,1998,179～213,227～230.
[2] 景可,卢金发,梁季阳.黄河中游侵蚀环境特征和变化趋势[M].郑州:黄河水利出版社,1998,1～33,93～108.
[3] 朱照宇,丁仲礼.中国黄土高原第四纪古气候与新构造演化[M].北京:地质出版社,1994,5～165.
[4] 黄培华.中国第四纪时期气候演变的初步探讨[J].科学通报,1963(1):34～39.
[5] 徐钦琦.地球轨道与气候演变的关系[J].科学通报,1990,25(3):180～182.
[6] Liu Tungsheng et al..Loess and the Environment[M].Beijing:China Ocean Press,1985.1～251.
[7] 中国科学院黄土高原综合科学考察队.黄土高原地区土壤侵蚀区域特征及其治理途径[M].北京:中国科学技术出版社,1990,92～156.
[8] 丁仲礼,刘东生,刘秀铭,等.250万年以来的37个气候旋回[J].科学通报,1989,34(19):1 494～1 496.
[9] Ding Zhongli,Yu Z,Rutter N W et al..Towards on orbital time scale for Chinese loess deposits[J].Quart.Sci.Rev..1994 (13):39～70.
[10] Zeitler P K,Johnson N M,Naeser C W et al..Fission track evidence for Quaternary of the Nanga Paibat[J].Pakistan.Nature,1993,398:255～257.
[11] 丁林,钟大赉,潘裕生,等.东西马拉雅构造与上新世以来快速抬升的裂变径迹证据[J].科学通报,1995(40):1 497～1 500.
[12] 李吉均.中国第四纪冰期、地文期和黄土记录[J].第四纪研究,1989(3):269～278.
[13] 丁仲礼,刘东生,刘秀铭,等.中国黄土的土壤地层与第四纪气候旋回[A].见:黄土*第四纪质*全球变化(第一集),北京:科学出版社,1990,1～26.
[14] 安芷生,S.Porter,G.Kukla等.最近13万年黄土高原季风变迁的磁化率证据[J].科学通报,1990,35(7):529～532.
[15] 安芷生.最近2万年中国环境变迁研究[A].见:黄土·第四纪地质·全球变化,北京:科学出版社,1990,1～26.
[16] 安芷生,吴锡浩,汪品先,等.最近130 ka中国的古季风(1.古季风记录)[J].中国科学(B):1991,(10):1076～1081.
[17] 安芷生,吴锡浩,汪品先,等.最近130 ka中国的古季风(1.古季风记录)[J].中国科学(B),1991,(11):1209～1215.
[18] 石建省,立铮华,魏明建,等.黄土与古气候演化[M].北京:地质出版社,1998,107～116.
[19] 赵景波.西北黄土区第四纪土壤与环境[M].西安:陕西科学技术出版社,1994,28～90,131～159.
[20] 吴锡浩,王富葆,安芷生,等.晚新生代青藏高原隆升的阶段和高度[A].见:黄土·四纪地质·全球变化(第三集).北京:科学出版社,1992,1～13.
[21] 张林源.青藏高原上升对我国第四纪环境的影响[J].兰州大学学报(自然),1981(3):142～155.
[22] 吴锡浩.青藏高原隆升幅度的初步研究[A].见:黄土*第四纪地质*全球变化.北京:科学出版社,1996.1～17.
[23] 郭其蕴,叶维明.南北半球大气环流与东亚季风[J].气象学报,1979,37(1):86～95.
[24] 安芷生,魏兰英,卢演俦.洛川黄土剖面土壤地层学的初步研究[J].中国第四纪研究,1985,6(1):166～174.
[25] 朱照宇.中国黄土高原及邻区水系沉积物-古土壤系列[J].科学通报,1989,34(6):446～449.
[26] 朱照宇.黄河中游河流阶地的形成与水系演化[J].地理学报,1989,44(4):441～452.
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备注/Memo
收稿日期:1999-12-18
基金项目:中国科学院“西部之光”项目资助
作者简介:李裕元(1965- )，男，河南博爱人，讲师，在读博士.主要从事土壤物理、水土资源与环境等方面的研究工作.