1)Holocene Megathermal全新世大暖期
1.A Method on Determining the Parameters of the Hydrological and Energy- Balance Model and Its Use: A Case Study of Qinghai Lake at Holocene Megathermal;水能联合方程恢复流域古降水量时参数的确定方法及其应用──以青海湖全新世大暖期古降水量推算为例
2.The Result indicated that the Holocene Megathermal climate is unstableness and there are several times dried events.通过对渭南北刘村黄土剖面的野外考察和粒度、磁化率、碳酸钙的分析,探讨了该地区全新世大暖期气候的高分辨率变化。
3.Acccording to pollen record and ~(14)C－dating in Zoige，located in the northeastern part ofthe Tibetan Plateau，this paper suggests that the Holocene megathermal took place about 9-3ka BP，when vegetation was coniferous and deciduous broad-leaf mixed forest，showing，awarmer and wetter climate in this region.本文通过对若尔盖黑河牧场ＤＣ剖面系统的孢粉分析，结合￣（１４）Ｃ测年，提出该区全新世大暖期发生于９－３ｋａＢＰ，当时的植被为针阔叶混交林，气候温湿。
英文短句/例句
1.Paleoclimate Fluctuations Analysis of Hainan Islands after Holocene Warm Period海南岛全新世大暖期后的古气候波动分析
2.Comparative Analysis on the Environmental Changes and Human-land Relationship between the Western Liaoning and Loess Plateau in Holocene Megathermal;全新世大暖期辽西与黄土高原地区环境演变及人地关系比较研究
3.The high resolution climatic study of the holocene megathermal in Beiliu Profile in Eastern Guanzhong Basin;关中盆地东部北刘剖面全新世大暖期气候高分辨率研究
4.The Holocene Megathermal in China with the Agricultural Civilization in the Middle and Lower Reaches of the Yellow River;中国全新世大暖期与黄河中下游地区的农业文明
5.Researches on Coastal Storm Surge Frequency during the Warm Period of Middle Holocene in Middle Jiangsu Province江苏中部海岸全新世中期温暖期风暴潮频率的研究
6.Regional division of the agricultural culture in the Holocene warm period in China and the relationship of human and environment中国全新世暖期农业考古文化分区及人地关系特征
7.An Analogy Analysis of Summer Precipitation Change Patterns Between Mid-Holocene and Future Climatic Warming Scenarios over East Asia中全新世暖期与未来气候变暖情景下东亚夏季降水变化相似型分析
8.Analysis on the Environment Change in the Early Period of the Late Holocene in Hebei Province华北地区晚全新世初期环境变化分析
9.Perspective for China s Resource Security in the Early of New Century;新世纪前期中国“资源安全”问题透视
10.The Temperature Characteristics of the Spatial Distribution and Temporal Evolution in China During the MWP中国中世纪暖期温度的时空变化特征
11.Adaptive Changes of Hunter-Gatherers during the Late Pleistocene-Early Holocene Transition in China;中国晚更新世—早全新世过渡期狩猎采集者的适应变迁
12.Holocene high beachrocks in South China and the strcture of coastal large earthquakes华南全新世高海滩岩与海岸大震构造
13.Holocene slip rate of the Wasatch fault zone, Utah, from geodetic data: earthquake cycle effects由大地测量数据得到的犹他州沃萨奇断层带的全新世滑动速率:地震周期效应
14.Point two: Totally new exqusite fitment, with terrestrial heat!! The first choice of family living!!!亮点二：全新精致装修，带地暖！！居家首选！！！
15.The installation of a new heating system will take two weeks.新暖气系统的安装需要两个星期。
16.During the Pleistocene Ice Age, the ancient drainage systems were almost completely rearranged by glaciation.在更新世冰期，古水系常被冰川作用完全改造。
17.Mid-holocene Climate Variation from Lake Evidences of East Asian Monsoon Margin Areas;季风边缘区全新世中期气候变化的古湖泊记录
18.A TANG DYNASTY MAP OF THE ERHAI LAKE OF CHINA AND THE CHANGE HISTORY OF WATER SYSTEM OF THE LAKE SINCE THE MID-HOLOCENE;唐《西洱河图》与全新世中期以来洱海水系变迁
相关短句/例句
Holocene warm period全新世暖期
1.Regional division of the agricultural culture in the Holocene warm period in China and the relationship of human and environment中国全新世暖期农业考古文化分区及人地关系特征
3)the Holocene Megathermal in China中国全新世大暖期
1.The Holocene Climatic Optimum is equal to the Holocene Megathermal in China,or the Yangshao Warm Period in China,it is about 8500～3000 years ago.距今8500~3000年是全新世以来气候最佳适宜期,在我国称之为“中国全新世大暖期”或“仰韶温暖期”。
4)stable wet and warm period in Holocene全新世暖湿期
5)mid-Holocene全新世中期
1.The Originatio Study of Mid-Holocene Sand Bed in Zhangbei,Northern Hebei Province;河北省北部张北县一带全新世中期砂层的成因
2.Mid-Holocene Climate Change in JingNing, GanSu Province;甘肃静宁地区全新世中期气候变化
6)Late Holocene全新世晚期
1.Compostion of Carbon Isotopes in Soil Carbonates and Paleoclimate Recoreds of The Late Holocene in the West of Jilin,China;吉林西部全新世晚期土壤碳酸盐中碳稳定同位素记录的古气候信息
2.A detailed record of sea level changes during the Late Holocene is preserved in the coastal environment of Fildes Peninsula, where 6 coral reef terraces were found.从而建立了全新世晚期南极菲尔德斯半岛的海平面变化序列 :在 430 0～ 2 430aBP期间 ,区域海平面快速下降 ,其平均下降速率为 - 0 6 0cm·a-1;在 。
3.This paper researched the origin of shell ridges in the coastal area of Tianjin and preliminarily determined the late Holocene age of their formation.本文通过对天津滨海贝壳堤成因的研究,初步确定贝壳堤是全新世晚期形成的,它的形成和演化反映了近岸生源物质迁移、现代沉积过程,贝壳堤的演化模式划分为三个阶段。
延伸阅读
暖答世1.蒙古语。元代称帝王受佛戒的仪式。
