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1)  climatic stratigraphy
气候地层
1.
Analyses of the two boreholes include OSL and U-series dating,pollen and microfossils,tending to reconstruct the high resolution climatic stratigraphy,and therefore to define the chronostratigraphy of the Late Quaternary.
根据对长江三角洲地区两个以细颗粒沉积为主的晚第四纪钻孔进行OSL测年、U系测年、孢粉分析和微体古生物分析,试图建立高分辨率气候地层,从而建立本区晚第四纪的年代地层框架,并探讨本区晚第四纪的标志层和期间发生的两次海侵及其机制。
2.
Based on this information,the lithostratigraphy,biostratigraphy and climatic stratigraphy since Late Pleistocene in the North China Plain had been further studied,the age borderline between Holocene and Pleistocene of the North China Plain had been determined.
在此基础上,对华北平原晚更新世以来的岩石地层、生物地层及气候地层进行了进一步的研究,厘定了华北平原全新世与晚更新世地层的年龄界线。
2)  climatic stratification
气候地层法
3)  climatostratigraphic classification
气候地层划分
1.
In view of negativity of Quaternary glaciation from eastern China, the author suggests; (l) not to use climatostratigraphic classification for Quaternary system in eastern China, (2) to use the term of diamictite instead of till in lithostratigraphic units,(3) Geographic names should be derived from permanent natural or artifical features which the stratigraphic unit is present.
中国东部第四纪冰川学说存在不肯定性暴露了气候地层划分和冰川地层单位命名的脆弱性。
4)  climate stratigraphic unit
气候地层单位
5)  geologic climate unit
气候-地层单元
6)  climate sequence
气候层序
1.
Two kinds of revolutionary models for sequences including structural sequence model and climate sequence model developed in foreland basin were presented.
研究结果表明,前陆盆地内发育有两种层序模式,即构造层序和气候层序。
2.
The model of the development of the climate sequence is put forward.
对存在于塔里木盆地志留-泥盆系台盆区的气候转变进行了深入分析,总结了气候在可容空间变化中的作用和以气候为主控因素的层序发育模式,提出了"气候层序发育模式",并且分析了气候层序发育过程中气候对层序发育的控制过程。
补充资料:东北平原农业气候资源利用(见农业气候资源利用)


东北平原农业气候资源利用(见农业气候资源利用)


  默军爵攫戳猛罚胃植和l用2 iyuanl心yong 见农业气候资
  
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