收稿日期: 1997-04-11
修回日期: 1997-11-15
网络出版日期: 1998-06-01
ADVANCES IN THE RESEARCH ON ORBITAL FORCING SEDIMENTARY RHYTHM—A DISCUSSION ON THE IMPLICATIONS TO SEDIMENTOLOGY, CHRONOLOGY AND STUDYING METHODS
Received date: 1997-04-11
Revised date: 1997-11-15
Online published: 1998-06-01
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 . DOI: 10.11867/j.issn.1001-8166.1998.03.0217
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.
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