1) 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
2) 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。
3) stable wet and warm period in Holocene
全新世暖湿期
4) 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”。
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。
补充资料：暖答世
1.蒙古语。元代称帝王受佛戒的仪式。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条