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地球科学进展  1998, Vol. 13 Issue (3): 217-224    DOI: 10.11867/j.issn.1001-8166.1998.03.0217
干旱气候变化与可持续发展     
地球轨道旋回沉积节律研究进展——兼论轨道旋回的沉积学特征、年代学意义和研究方法
柳永清
中国科学院地质研究所 北京 100029
ADVANCES IN THE RESEARCH ON ORBITAL FORCING SEDIMENTARY RHYTHM—A DISCUSSION ON THE IMPLICATIONS TO SEDIMENTOLOGY, CHRONOLOGY AND STUDYING METHODS
Liu Yongqing
Geology Institute, CAS, Beijing 100029
 全文: PDF(252 KB)  
摘要:

地球轨道旋回是古代沉积记录中常见的由地球轨道参数变动控制的沉积节律,它不仅自身表现显著的节律性,而且通过反馈体系强烈影响着沉积作用。同时,轨道旋回节律在不同的沉积背景下以不同的沉积特征显现和规则性叠加。地球轨道旋回赋有的规则频率变化特征又使其具有年代学意义和应用价值,它是天文地质学、地层学及沉积学研究的重点内容。根据国内外资料综述了这些方面的研究进展,并探讨了地球轨道旋回的研究方法。

关键词: 地球轨道旋回沉积学年代学研究方法    
Abstract:

The orbital forcing cycles, i.e., Milankovitch cycles, are common sedimentary rhythms presented within the ancient deposits, which is key subjects in astrogeology,stratigraphy and sedimentology. Since 19th century, a cyclicity orrhythm of eccentricity,obliquity and precession of Earth orbital paths has been discovered and widely discussed by the researchers all the world. A mechanics of orbital forcing climate cycle, which has a strong effect on depositional sequences through the albedo systems, was focused in a variety of case studies from Quaternary to Precambrian records. The orbital cycles not only display a rhythm itself, but also control depositional stacked patterns, i.e., sedimentary rhythms, from deep sea to tidal settings. Since orbital forcing cycles are characterized by a variation of frequency they have an implication of chronology and give a high resolution durations of stratigraphy, depositional sequences, geological events and biota zones etc. This paper gives a general reviews of the advances in research on orbital cycles, and an approach to the study, including mathem tics and geology based on the studies abroad and home.

Key words: Orbital forcing cycle    Sedimentology and chronology    Study methods.
收稿日期: 1997-04-11 出版日期: 1998-06-01
:  P53  
通讯作者: 柳永清   
作者简介: 柳永清,男,1960年6月出生, 助理研究员, 主要从事沉积地质学和事件地质学等的研究。
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引用本文:

柳永清. 地球轨道旋回沉积节律研究进展——兼论轨道旋回的沉积学特征、年代学意义和研究方法[J]. 地球科学进展, 1998, 13(3): 217-224.

Liu Yongqing. ADVANCES IN THE RESEARCH ON ORBITAL FORCING SEDIMENTARY RHYTHM—A DISCUSSION ON THE IMPLICATIONS TO SEDIMENTOLOGY, CHRONOLOGY AND STUDYING METHODS. Advances in Earth Science, 1998, 13(3): 217-224.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.1998.03.0217        http://www.adearth.ac.cn/CN/Y1998/V13/I3/217

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