中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Origin of the Miocene-Pliocene Red-Earth formation at Xifeng in northern China and implications for paleoenvironments

文献类型:期刊论文

作者Guo, ZT; Peng, SZ; Hao, QZ; Biscaye, PE; Liu, TS
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
出版日期2001-06-01
卷号170期号:1-2页码:11-26
关键词Red-Earth Red-Clay eolian deposits Asian aridification Loess Plateau pliocene
ISSN号0031-0182
文献子类Article
英文摘要In the eastern Loess Plateau region of northern China, the Quaternary loess-soil sequences of the last 2.6 Ma are underlain by the Hipparion Red-Earth Formation. Magneto-stratigraphic studies suggest that it is a near continuous terrestrial record for the period from similar to7 to similar to2.6 Ma BP, and therefore, has great potential for the study of Asian paleoclimates. The origin of this formation is controversial and needs further study. In this work, the Xifeng Red-Earth section, a type section for the eastern Loess Plateau region, was studied using optical microscopic analysis, grain-size measurements, and both major- and trace-element geochemical properties to address questions of its origin and environmental implications. The results show that this formation consists of three parts. The Lower part (>6.2 Ma BP) is a water-reworked deposit related to alluvial and slope processes; the Middle part (from similar to6.2 to similar to3.6 Ma BP) was derived from in situ eolian dust deposition, but was significantly affected by groundwater oscillations; and the Upper part (from similar to3.6 to similar to2.6 Ma BP) is an eolian formation, similar to the Quaternary loess-soil sequence. The grain-size of the Upper part is significantly coarser than for the middle part, but finer than for the overlying loess.
WOS关键词LOESS PLATEAU ; PALEOCLIMATIC IMPLICATIONS ; ASIAN MONSOON ; MAGNETOSTRATIGRAPHY ; CLIMATE ; SEQUENCES ; STRATIGRAPHY ; HEMISPHERE ; ATLANTIC ; UPLIFT
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
WOS记录号WOS:000169441700002
出版者ELSEVIER SCIENCE BV
源URL[http://ir.iggcas.ac.cn/handle/132A11/76443]  
专题中国科学院地质与地球物理研究所
通讯作者Guo, ZT
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.State Key Lab Loess & Quaternary Geol, Xian 710054, Peoples R China
3.Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
推荐引用方式
GB/T 7714
Guo, ZT,Peng, SZ,Hao, QZ,et al. Origin of the Miocene-Pliocene Red-Earth formation at Xifeng in northern China and implications for paleoenvironments[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2001,170(1-2):11-26.
APA Guo, ZT,Peng, SZ,Hao, QZ,Biscaye, PE,&Liu, TS.(2001).Origin of the Miocene-Pliocene Red-Earth formation at Xifeng in northern China and implications for paleoenvironments.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,170(1-2),11-26.
MLA Guo, ZT,et al."Origin of the Miocene-Pliocene Red-Earth formation at Xifeng in northern China and implications for paleoenvironments".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 170.1-2(2001):11-26.

入库方式: OAI收割

来源:地质与地球物理研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。