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1)  eolian sequence
风积序列
2)  aeolian dust deposition paleosol sequence
风尘堆积-古土壤序列
1.
As a paleo climatic proxy index, magnetic susceptibility parameter, which has been widely used in the loess studies of northern China, is applied in the studies on quaternary aeolian dust deposition paleosol sequence located in the south of the lower reaches of the Yangtze River.
将北方黄土研究中广泛应用的磁化率参数引入江南第四纪风尘堆积区研究,对安徽宣城风尘堆积-古土壤序列向阳剖面进行了系统的磁化率化采样、测试,根据该剖面磁化率及其曲线的变化特征,对其古气候指示意义进行了初步的探讨。
3)  depositional sequence
沉积序列
1.
Based on the bore section, combining with the study on lithology, well logging, seismic facies and sequence type, the structure of the sequence in the deeply down-faulted Dongying Sag is analyzed emphasizing on the low-stand fan depositional type, its controlling factors and depositional sequence.
以钻井剖面相分析资料为基础,结合岩性、测井、地震响应特征及层序类型分析,研究东营凹陷深陷期层序的构成,着重探讨其中低位扇的沉积相类型、发育的控制因素及沉积序列。
2.
On the basis of an analysis of the characteristics of Quaternary depositional sequences and sporopollen assemblages in the Gonghe basin,combined with the thermoluminescent dating,the authors have studied the environmental change in the basin since the Quaternary and divided the change into two major phases:the early .
通过对共和盆地第四系沉积序列特征和孢粉组合特征的分析,结合热释光测年,本文较详细地研究了共和盆地第四纪以来的环境变迁,并将其分为两大阶段:早期为湖相沉积阶段(中更新世晚期~0 079Ma),气候相对温和。
3.
It can be divided into 3 depositional sequences(succession of strata), i.
可划分为三个沉积序列(层序)。
4)  sedimentary sequence
沉积序列
1.
Description of Cretaceous sedimentary sequence of the Yaojia Formation recovered by CCSD-SK-Ⅰs borehole in Songliao Basin:Lithostratigraphy,sedimentary facies and cyclic stratigraphy
松科1井南孔白垩系姚家组沉积序列精细描述:岩石地层、沉积相与旋回地层
2.
Description of Cretaceous sedimentary sequence of the second and third member of the Qingshankou Formation recovered by CCSD-SK-Ⅰs borehole in Songliao Basin:Lithostratigraphy,sedimentary facies and cyclic stratigraphy
松科1井南孔白垩系青山口组二、三段沉积序列精细描述:岩石地层、沉积相与旋回地层
3.
Description of Cretaceous sedimentary sequence of the first member of the Qingshankou Formation recovered by CCSD-SK-Ⅰs borehole in Songliao Basin:Lithostratigraphy,sedimentary facies and cyclic stratigraphy
松科1井南孔白垩系青山口组一段沉积序列精细描述:岩石地层、沉积相与旋回地层
5)  strata accumulation series
垒积序列
6)  product sequence
乘积序列
补充资料:风积作用
当风速减小时,风力减弱,风所挟带的沙粒等物质发生堆积的作用。堆积物质称为风积物,主要为沙和黄土。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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