1)Mid-Holocene中全新世
1.Evolution of Mangrove Forests in Northeastern Hainan Island Since Mid-Holocene;海南岛东北部中全新世以来红树林的演化
2.Paleo-Hydrological Signification in Mid-Holocene Revealed by the Analysis of Soluble Salts of Sihenan Profile in Mengjin,Henan Province;河南孟津寺河南中全新世湖泊沉积物的易溶盐测定及其古水文意义
3.The Mid-Holocene Climate Simulated by a Grid-Point AGCM Coupled with a Biome Model;用一个耦合的全球格点大气环流模式——植被模式模拟中全新世气候变化(英文)
英文短句/例句
1.MM5 simulations of the China regional climate during the mid-HoloceneMM5对中全新世时期中国地区气候的模拟研究
2.The New Century World Structure in the Process of Economic Globalization;经济全球化进程中的新世纪世界格局
3.Economic Globalization and Chinese Cultural Trend in the New Century论经济全球化与新世纪中华文化走向
4.Climatic change and environmental characteristic of Holocene in North China;全新世中国北方气候变化及环境特征
5.Philosophy of the Economic Security of China under of New Political Situation in the World;世界政治新形势下的中国经济安全观
6.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
7.Neo-globalization and China s Social Development in the 21st Century;新全球化与21世纪中国社会发展论纲
8.On the Progress of Chinese Literature in the New Century;“两全”背景下中国新世纪文学进展论纲
9.Globalization:Chinese Fine Art Education Facing with New Century;全球化:挑战新世纪的中国美术教育
10.The Climatic Change during the Holocene in Southern Weihe River of the Guanzhong Area关中渭河以南地区全新世的气候变迁
11.THE REFLECTIONS OF GLOBAL TECTONICS EVENTS AT THE PALEOCENE EOCENE BOUNDARY IN SEDIMENTOLOGY古新世—始新世界线全球构造事件在沉积学中的反映
12.Chemical Element Distribution and Palaeoclimate in Late Pleistocene-Holocene Strata in East Gonghe Basin青海共和盆地东部晚更新世——全新世地层中元素分布与古气候
13.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
14.Plio-Miocene beds上新世-中新世地层
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16.The Holocene Paleosol and Soil Moisture Environment in Guanzhong Plain;关中平原全新世土壤和土壤水环境研究
17.Holocene Environmental Change of Pedogenensis in the Middle Reaches of the Jinghe River Basin;泾河中游地区全新世成壤环境演变研究
18.Changes in Holocene Terrestrial Carbon Storage over China;全新世中国陆地生态系统碳储量的初步估算
相关短句/例句
Middle Holocene中全新世
1.Evironmental evolvement of the north branch of the Changjiang estuary since middle holocene;中全新世以来长江口北支环境的演变
2.Environmental Change and Its Impact on Human Activities in Middle Holocene at Mengjin, Henan Province;河南孟津地区中全新世环境变化及其对人类活动的影响
3.Cultural evolution and its environmental force in middle holocene at Guanzhong-Shanbei-Longdong Region,China;中全新世关中陕北陇东地区文化演变及环境驱动力
3)Mid Holocene中全新世
1.Mid Holocene Paleoclimatic Paleoenvironmental Changes in Zhejiang Province and Hemudu Ancients;浙江中全新世古气候古环境变化与河姆渡古人类
2.The palaeoclimate driven vegetation has been simulated by biome models showing the mid Holocene forest vegetation was shifted southwards in China.地球轨道参数驱动的太阳辐射变化造成了中全新世北半球大陆夏季的普遍增温 ,但中低纬度的冬季温度低于现代。
4)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
5)Middle Holocene全新世中期
1.A preliminary study oa the environmental change and cultural evolution in Middle Holocene in Gansu-Qinghai Region;甘青地区全新世中期的环境变化与文化演进
6)mid to late Holocene中晚全新世
延伸阅读
全新世全新世HoloceneEpach地质时代的最新阶段，第四纪二分的第二个世，开始于12000～10000年前持续至今。这一时期形成的地层称全新统，它覆盖于所有地层之上。全新世是1850年P.热尔韦提出的，并为1885年国际地质大会正式通过。全新世时间短，沉积物厚度小，但分布范围广。由于距今时代短，可应用几种有效的年代测定方法，因此，其地层划分比较详细、精确。全新世与更新世的界限，以第四纪最后一次冰期结束、气候转暖为标志，因此又称为冰后期。全新世气候有轻微波动。海面变化与气候相一致，冰后期海面迅速上升，到距今11000年上升到－60米位置。距今6000年海面已接近现今位置，其后仅有轻微的变化。全新世时，人类进入现代人阶段。
