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摘要:
Experiments on stratification discussed here have revealed the mechanical nature of lamination as well as the role of turbulent current as agent of stratification. They challenge Steno’s principle that superposed strata are successive sedimentary layers. They show that relative chronology should not be referred to as “stages” but as “sequences” of series. The rock formation studied by Lalomov shows that the duration of sedimentation could be considerably shorter than indicated by the Geological Time Scale. The latter scale corresponds to large marine transgressions and regressions that can result from the shift of polar axis following such major orogeneses as the Caledonian, Hercynian and Alpine.
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篇名 Orogenesis: Cause of Sedimentary Formations
来源期刊 地质学期刊(英文) 学科 医学
关键词 STRATIFICATION LAMINATION TURBULENT Flow Time of SEDIMENTATION OROGENESIS
年,卷(期) 2013,(2) 所属期刊栏目
研究方向 页码范围 22-24
页数 3页 分类号 R73
字数 语种
DOI
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研究主题发展历程
节点文献
STRATIFICATION
LAMINATION
TURBULENT
Flow
Time
of
SEDIMENTATION
OROGENESIS
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研究来源
研究分支
研究去脉
引文网络交叉学科
相关学者/机构
期刊影响力
地质学期刊(英文)
月刊
2161-7570
武汉市江夏区汤逊湖北路38号光谷总部空间
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585
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0
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