晚新生代,Late Cenozoic
1)Late Cenozoic晚新生代
1.Late Cenozoic structural deformation and its implication for petroleum accumulation in the southern Junggar thrust belt;准南地区前陆冲断带晚新生代构造变形特征与油气成藏
2.Late Cenozoic squeezing out tectonism in Qinghai Tibet Plateau and its impactson late hydrocarbon accumulation in rift basins in eastern China;晚新生代青藏高原构造挤出及其对中国东部裂陷盆地晚期油气成藏的影响
3.Issues onLate Cenozoic red-earth in northern China;中国北方晚新生代红粘土研究之若干问题
英文短句/例句
1.The Study on the Late Cenozoic Environment Change of Linfen Basin, Shanxi Province山西临汾盆地晚新生代环境演变研究
2.Glacial Period Divisions and Palaeoglacial Problems of Late Cenozoic Age in Guizhou贵州晚新生代冰期划分与古冰川问题
3.Environmental Evolution at the Drilling Hole K3 in the East-south Margin of Ebinur Lake,Xinjiang in Late Cenozoic新疆艾比湖东南缘K3孔晚新生代环境演化
4.An exploration to the theory and methodology of Late Cenozoic geological mapping晚新生代地质填图理论与方法的新探索
5.Formation and Evolution of the Middle Reaches of the Yellow River Since Late Cenozoic黄河中游晚新生代地貌演化与黄河发育
6.EVOLUTION OF THE LATE CENOZOIC DEPOSITIONAL ENVIRONMENTS IN THE KUNMING BASIN, YUNNAN云南昆明盆地晚新生代沉积环境的演化
7.PRELIMINARY ANALYSIS OF TECTONIC EVILUTION OF TAIXINAN BASIN IN LATE CENOZOIC台西南盆地晚新生代构造演化初步分析
8.Genetic Types And Mineralization Law Of Minerals Resources Of Late Cenozoic In Guizhou贵州晚新生代矿产资源成因类型和成矿规律
9.ANALYSING THE ENVIRONMENTAL EVOLUTION OF LINFEN-HUOMA BASIN IN THE LATE CENOZOIC ERA WITH THE METHOD OF SPORO-POLLEN用孢粉方法分析临侯盆地晚新生代环境演变
10.The Characteristics of Tectonics and Hydrocarbon Accumulation of Jizhong Depression in late Cenozoic era冀中坳陷晚新生代地质构造特征及其油气赋存
11.DEFORMATION CHARACTERISTICS AND DISPLACEMENT AMOUNT OF THE LIANGSHAN ACTIVE FAULT ZONE IN LATE CENOZOIC ERA凉山活动构造带晚新生代变形特征与位移规模
12.LATE CENOZOIC ERA SEDIMENT AND ACTIVITY OF THE JIANGSU SEGMENT OF THE TAN-LU FAULT ZONE郯庐断裂带江苏段晚新生代沉积与断裂活动
13.There are at least nine physiographic cycles in the middle reaches of the Yellow River during the Late Cenozoic Era.在晚新生代黄河中游至少存在九个地文期旋回。
14.Tectonic Significance of Sedimentary Record in Northern Edge of Altyn Tagh Range;阿尔金山北麓晚新生代沉积记录的构造意义
15.Sediment Character of Xigeda Formation and the Paleoenvironmental Implication Since Late Cenozoic in the West of Sichuan;川西晚新生代昔格达组沉积特征及古环境意义
16.Possible provenances and their change of aeolian deposits in north China in late Cenozoic;晚新生代中国北方风尘沉积的可能物源及变化
17.Discussion on Several Typical Late Cenozoic Stratigraphic Units in North China华北地区晚新生代几个地层单元的讨论
18.THE LATE CENOZOIC DEFORMATION OF THE WUSUNSHAN MOUNTAIN IN THE YILI BASIN AND ITS SIGNIFICANCE伊犁盆地南部乌孙山晚新生代变形特征及意义
相关短句/例句
Late Cenozoic新生代晚期
1.According to these data together with the sporopollen assemblage data from the Xining-Minhe basin, Lunpola basin, Namlin basin and Weihe basin, the authors analyzed the evolution of theLate Cenozoic paleovegetations and paleoenvironment on the Qinghai-Tibet Plateau and in its a.对取自沱沱河盆地、通天河盆地、那曲盆地、东温泉盆地、乌郁盆地的新近纪湖相沉积与取自巴斯错、错鄂、纳木错的晚第四纪湖相沉积,进行孢粉分析;结合西宁—民和盆地、伦坡拉盆地、南木林盆地、渭河盆地的孢粉资料,分析青藏及邻区新生代晚期古植被和古环境的演化过程。
3)Late Mesozoic-Cenozoic晚中生代-新生代
1.Division of the Tectonic Sequences and Tectonic Evolution ofLate Mesozoic-Cenozoic in Weatern Qinling;西秦岭晚中生代-新生代构造层划分及其构造演化过程
4)Late Cenozoic tectonic movement晚新生代构造
1.Late Cenozoic tectonic movement in the Keyir Mountain area,Kuqa,Xinjiang,and its controls on sandstone-type uranium deposits;新疆库车黑英山地区晚新生代构造运动及其对砂岩型铀矿成矿的控制作用初析
5)Environment in late Cenozoic晚新生代环境
6)Late Cenozoic strata晚新生代地层
延伸阅读
晚新生代大冰期又称第四纪大冰期。晚新生代发生大规模冰川作用的时期。第三纪中期，全球气候开始转冷，自然地理带向中低纬度带及海拔低处推移，极地冰盖范围扩大，中低纬度的高山也发生冰川作用。除南极冰期始于第三纪中期外，其余地区多属第四纪冰期，距今24o万年前至距今1万年前。第四纪冰期的冰川规模很大，北半球大冰盖的南缘在欧洲抵达北纬50°左右，在北美大陆一直推进到北纬40°以南；南极洲的冰盖也比现今大得多。据估计，在晚更新世末次冰期的最盛时期，世界大陆有32％的面积被冰川覆盖，冰川总面积为现今的3倍，海平面下降130米左右，气温较今低3～7～11℃。第四纪大冰期的来临，对自然环境的演变及人类的进化部产生重大影响。
