1) Late Mesozoic-Cenozoic
晚中生代-新生代
1.
Division of the Tectonic Sequences and Tectonic Evolution of Late 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
2) 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 impacts on 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 on Late Cenozoic red-earth in northern China;
中国北方晚新生代红粘土研究之若干问题
3) late Mesozoic
晚中生代
1.
Strata Sequence of the Late Mesozoic and Basin Evolution in the Southeastern Liaoning;
辽东南地区晚中生代地层序列与盆地演化规律
2.
A new case of Late Mesozoic crust-mantle interaction in eastern Zhejiang:Geochronology and geochemistry of the Ru ao diabase-granite composite intrusions;
浙东晚中生代壳幔相互作用的新例证——新昌儒岙辉绿岩-花岗岩复合岩体的年代学与地球化学
3.
A review on the late Mesozoic extensional tectonics on the eastern North China Craton;
华北东部晚中生代伸展构造作用
4) Late Palaeozoic-Mesozoic
晚古生代-中生代
5) 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 the Late 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。
6) Late Mesozoic
中生代晚期
1.
Late Mesozoic and Paleogene Basalts and Deep-Derived Xenocrysts in Eastern Liaoning Province, China: Constraints on Nature of Lithospheric Mantle;
辽东中生代晚期和古近纪玄武岩及深源捕虏晶——对岩石圈地幔性质的制约
2.
Division of the Late Mesozoic strata in Zhejiang;
论浙江中生代晚期地层划分
3.
Taxonomy of Fossil Ephemeroptera from Late Mesozoic in China, with Comments on Succession of Aquatic Insect Community
中国中生代晚期蜉蝣目化石研究及水生昆虫群落演替分析
补充资料：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。
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