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DOI:
地质力学学报:2002,8(4):369-375
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安徽宣城黄土堆积的磁性地层学与古环境意义
(1.中国科学院地质与地球物理研究所, 北京 100029;2.中国科学院地球环境研究所, 西安 710005;3.北京大学, 城市环境学院 100871)
MAGNETOSTRATIGRAPHY AND PALEOCLIMATIC SIGNIFICANCE OF AN EOLLIAN SEQUENCE FROM THE XUANCHENG AREA,ANHUI PROVINCE
(1.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China;2.Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710005, China;3.Academy of Urban Environment, Beijing University, Beijing 100871, China)
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投稿时间:2002-09-13    
中文摘要: 利用磁性地层学方法对安徽宣城剖面的研究表明,B/M界限位于剖面中网纹红土的中下部,结合光释光测年可以外推出长江中下游地区的典型风成沉积开始形成于0.85Ma前后。这一年龄对应于一次全球性的气候转型事件,在海洋沉积与我国北方的黄土-古土壤序列中均记录了这一气候转型事件。同时,0.85Ma对应于中更新世的两大地质事件,一是全球冰量的增加,二是青藏高原的快速隆升,长江中下游地区风成堆积的开始,可能是上述两个因素共同作用的结果。
Abstract:A loess-soil sequence near Xuancheng from the Yangtze valley is investigated using magnetostratigraphy and luminescence dating to determine the location of B/M boundary.This boundary is found to be located within the middle-lower part of the so-called plinthitic laterite.,a widely distributed mid-Pleistocene tropical soils in southern China.The magnetostratigraphy data,combining with the OSL age suggests a basal age of the typical eolian depositional loess-soil sequence is about 0.85Ma.This age boundary corresponds to a significant global climate change,also is recorded in the marine sediments and in the loess-paleosol sequence in northern China.It also coincides with two geological events,intensive uplift of the Tibetan Plateau and the extension of the global ice volume.We interpret the onset of eolian loess deposition in the middle-lower reaches of Yangtze River as a result of hydrological and circulation changes associated with above two events occurring at the mid-Pleistocene.
文章编号:     中图分类号:P539.3    文献标志码:
基金项目:国家自然科学基金项目(编号:49894176)
引用文本:
乔彦松,郭正堂,郝青振,等,2002.安徽宣城黄土堆积的磁性地层学与古环境意义[J].地质力学学报,8(4):369-375.DOI:
QIAO Yan-song,GUO Zheng-tang,HAO Qing-zhen,et al,2002.MAGNETOSTRATIGRAPHY AND PALEOCLIMATIC SIGNIFICANCE OF AN EOLLIAN SEQUENCE FROM THE XUANCHENG AREA,ANHUI PROVINCE[J].Journal of Geomechanics,8(4):369-375.DOI:

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