Implication of Statistical Features of Terrace Pebbles to River Evolution from Baode County to Kehu Town

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  • MOE Laboratory for Earth Surface Processes and Department of Geography, Peking University, Beijing 100871

Received date: 2006-04-18

  Revised date: 2006-08-27

  Online published: 2007-07-20

Abstract

The lithology,grain size and orientation of the pebbles in different sites and on different river terraces have been studied along the Huanghe(Yellow) River from Baode to Kehu in the Shanxi-Shaanxi Gorge area.It is found that the pebbles are similar in lithology on different terraces in the same region,as well as on the same terrace from the upstream to the downstream.The grain sizes of limestone pebbles have a tendency of becoming smaller from upstream to downstream.This indicates the pebbles maybe the relics of the ancient Huanghe River.Because the highest pebbles are covered by late-Tertiary red clay,it is concluded that the Huanghe River run through this area at least in late Tertiary.

Cite this article

LIU Yun-Ming, LI You-Li, LU Hong-Hua, LI Xin-Po . Implication of Statistical Features of Terrace Pebbles to River Evolution from Baode County to Kehu Town[J]. SCIENTIA GEOGRAPHICA SINICA, 2007 , 27(4) : 567 -572 . DOI: 10.13249/j.cnki.sgs.2007.04.567

References

[1] 德日进,杨钟健.山西西部陕西北部蓬蒂纪后黄土期前之地层观察[J].地质专报,1930(甲种),(8):1~19.
[2] 王乃樑.对于张伯声先生"从黄土线说明黄河河道的发育"一文的意见[J].科学通报,1956,(7):67~72.
[3] 李容全.黄河的形成与变迁[A].见:杨景春.中国地貌特征与演化[M].北京:海洋出版社,1993.52~59.
[4] 袁宝印,王振海.青藏高原隆起与黄河地文期[J].第四纪研究,1995,(4):353~357.
[5] 李吉均,方小敏,马海洲,等.晚新生代黄河上游地貌演化与青藏高原隆起[J].中国科学(D辑),1996,26(4):316~322.
[6] Lin Aiming,Yang Zhenyu,Sun Zhiming,et al.How and when did the Yellow River develop its square bend[J].Geology,2001,29(10):951-954.
[7] 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):429~439.
[8] 程绍平,邓起东,闵伟,等.黄河晋陕峡谷河流阶地和鄂尔多斯高原第四纪构造运动[J].第四纪研究,1998,3:238~248.
[9] 潘保田,李吉均,曹继秀.黄河中游的地貌与地文期问题[J].兰州大学学报(自然科学版),1994,30(1):115~123.
[10] 杨东,方小敏,彭子成,等.陇西六盘山黄土及最近1.8MaB.P.以来的构造运动与气候变化[J].地理科学,2006,26(2):192~198.
[11] 张抗.黄河中游形成史初探[J].中国第四纪研究,1988,8(1):185~193.
[12] 潘保田,王均平,高红山,等.河南扣马黄河最高级阶地古地磁年代及其对黄河贯通时代的指示[J].科学通报,2005,50(3):255~261.
[13] 周春林,袁林旺,刘泽纯,等.南京汤山地区的地貌与岩溶发育演化[J].地理科学,2006,26(1):47~51.
[14] 郑朝贵,朱诚,高华中,等.南京江北地区晚更新世末期以来泥炭层δ13C记录的古气候变化[J].地理科学,2006,26(3):328~334.
[15] 朱丽东,叶玮,周尚哲,等.中亚热带第四纪红粘土的粒度特征[J].地理科学,2006,26(5):586~591.
[16] 胡春生,潘保田,高红山,等.最近150 ka河西地区河流阶地的成因分析[J].地理科学,2006,26(5):603~608.
[17] 胥勤勉,杨达源,葛兆帅,等.金沙江三堆子乌东德河段阶地研究[J].地理科学,2006,26(5):609~615.
[18] 高玄彧.地貌形态分类的数量化研究[J].地理科学,2007,27(1):109~114.
[19] 李景宜.陕西渭河下游湿地环境风险因素分析[J].地理科学,2007,27(3):71~375.
[20] 中国科学院《中国自然地理》编辑委员会.中国自然地理地貌[M].北京:科学出版社,1980.
[21] 马丽芳.中国地质图集[M].北京:地质出版社,2002.
[22] 杨达源,吴胜光,王云飞.黄河上游的阶地与水系变迁[J].地理科学,1996,16(2):137~143.
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