嵩山主峰的形成及演变

发布时间：2012-07-05 11:58:16 点击：700

《 成都理工大学学报：自然科学版 》Journal of Chengdu University of Technology: Sci & Technol Ed
起止页码：317-322
国际标准刊号：ISSN 1671-9727
国内统一刊号：CN 51-1634/N
嵩山主峰的形成及演变
李强 王梅英
郑州工业贸易学校地质矿产勘查系,郑州450007
摘　要:
对河南嵩山主峰的形成和演变过程进行了分析讨论。嵩山地区地层的分布、沉积岩的岩性特征、地层间的接触关系等证据，表明从古生代直至中生代嵩山并不存在。通过对嵩山山前新生代沉积盆地沉积和作为嵩山断块山和山前断陷盆地分界的君召-太后庙断层构造岩带的研究，证明现今的嵩山应当是在印支-燕山运动中孕育，在喜马拉雅运动中出生并长高的山脉。嵩山的成长过程可分为孕育、幼年、童年和青年阶段。嵩山在形成后主峰不断向北推移，推移距离达6．5km，隆起的铅直高度在7km以上。嵩山和中国大地其他山脉，如喜马拉雅山、天山、昆仑山、秦岭等，是同一辈份的年青山脉。[著者文摘]
关键词:
嵩山 造山运动 地层 山脉隆起
分类号:　P542[著者标引]
文献标识码：A
文章编号：1671-9727（2008）03-0317-06
栏目信息：地质与矿产勘探
相关文献:
主题相关 全文快照　　　
The formation and evolution of the highest peak of Mountain Songshan, Henan, China
LI Qiang, WANG Mei-ying
Department of Geology and Mineral Resources Prospecting, Zhengzhou School of Industrial and Trade, Zhengzhou 450007, China
Abstract:
Instead of forming in Paleozoic to Mesozoic, the highest peak of Mountain Songshan was gestated in Indosinian-Yanshanian movement, born and elevated during Himalayan movement. Evidences from the distribution of stratum, lithology of sedimentary and their contact relationships support this viewpoint. Based on the analyses of the Cenozoic foothill sedimentary basin in Mountain Songshan and the study of the Junzhao-Taihoumiao fault zone which is the boundary between fault block mountain and downfaulted basin in Songshan area, the authors belive that the formation of Mountain Songshan can be divided into four phases i. e. gestation, infancy, childhood and youth. The authors estimate that the highest peak of Mountain Songshan continuously moves towards north reach to 6. 5 km since its formation, and Mountain Songshan has uplifted more than 7 km since its naissance. So, as the same as Himalaya, Tianshan, Kunlun and Qinling mountains, Mountain Songshan is a young mountain.[著者文摘]
Key words:
Mountain Songshan; orogeny ; stratum; mountain＇ s uplift
收稿日期:　2006-12-14
修订日期:　
基金资助:
本文的电脑绘图由冷晓雷同志制作,在此特表谢意.
作者简介:
李强（1946-），男，教授，从事矿物岩石学及矿床学的教学与科研工作，E-mail：zzgmliqiang@sohu．com。