1) late pleistocene
晚更新世
1.
Characteristics of Palynological Assemblage of Late Stage of Late Pleistocene in Changjiang River Delta Area and Paleoenvironment;
长江三角洲地区晚更新世晚期的孢粉特征及古环境
2.
The Sporopollen Assemblages and Their Paleoenvironment Significance of the Qianhu Bay,Zhangpu,Fujian since Late Pleistocene;
福建漳浦前湖湾晚更新世的孢粉组合及其古环境意义
3.
The distribution of elephant fossils and the physiognomy characters of late Pleistocene in Jixian County of Tianjin;
天津蓟县晚更新世象化石分布与地貌特征
2) The late pleistocene
晚更新世
1.
Syn-depositional Deformation Structures by Earthquake Related to Volcanic Activity of the Late Pleistocene in Weizhou Island, Beihai City, Guangxi;
广西北海涠洲岛晚更新世火山活动引起的地震同沉积变形构造
2.
Deposit Characteristic and Developed Law of Debris Flow During the Late Pleistocene in Xiaojiang Valley;
晚更新世小江流域泥石流沉积特征及发育规律
3.
Based on the sporo-pollen analysis and ￣(14)C dating from Balikun Lake Core ZK024, the sporo-pollen assemblages array surbey in Balikun Basin since the late Pleistocene is drawn out, and six comprehensive sporo-pollen zones are divided.
本文根据巴里坤湖ＺＫ─０２４孔的孢粉分析结果和~（１４）Ｃ测年数据研究对比，总结归纳出巴里坤盆地晚更新世以来的孢粉组合序列概貌，并划分为六个孢粉组合带，在大陆性气候控制下的新疆，晚更新世以来干湿冷暖配置状况与东部地区相反。
3) late Pleistocene Epoch
晚更新世
1.
Late Pleistocene epoch lake facies sedimentary characteristics, paleoplant-cover and definition of climate transformation since 17.4 ka B.P.Tanggula area, Qinghai;
青海唐古拉地区晚更新世湖相沉积特征、古植被及17.4kaB.P.以来气候转型期的厘定
2.
late Pleistocene Epoch, early-middle Holocene Epoch and late Holocene Epoch.
从沉积学、孢粉学、年代学、矿物学和地球化学的角度,探讨了大、小兴安岭北部第四纪砂金矿的形成与演化,将砂金戍矿时代划分为3个主要时期:晚更新世、全新世早-中期和全新世晚期。
3.
It is considers that the activitie caused by tensile force at those faults such as Guangzhou-Conghua,Qingquanjie,Shougouling and Wenchong since Late Pleistocene Epoch,but the activity is weak relatively and without serious harms to engineering.
认为晚更新世以来 ,广从断裂、清泉街断裂、瘦狗岭断裂和文冲断裂发生过拉张式活动 ,但活动较弱 ,对工程地震未构成较严重危害 ,但在这些断裂所通过的地方存在砂土液化、淤泥塌陷等潜在的地质灾
4) late middle-Pleistocene
晚中更新世
1.
This paper analyzes the Luohe Rivers terraces, and the landform pattern which was reserved by the loess-palaeosol series in Luochuan loess plateau region since late middle-Pleistocene, and have obtained some conclusion.
通过分析洛川塬区晚中更新世以来洛河阶地和沟谷黄土、古土壤记录的古地貌形态得出,560～460kaB。
5) Late Pleistocene
更新世晚期
1.
The Comparisons of Cranial Non-metric Features between Upper Cave Skulls and Modern North Chinese Populations, and Late Pleistocene Human Evolution in China;
山顶洞人与现代华北人头骨非测量性特征比较及中国更新世晚期人类演化的一些问题
2.
Late Pleistocene Human Teeth Found in the Huanglong Cave,Yunxi of Hubei Province
湖北郧西黄龙洞更新世晚期人类牙齿
3.
The Huanglongdong Cave site (named "Yunxi Man Site"), which was discovered in 2004, is an important paleoanthropological site of Late Pleistocene in China.
湖北省黄龙洞“郧西人”遗址是2004年新发现的一处重要的更新世晚期古人类遗址。
6) mid-late Pleistocene
中-晚更新世
补充资料：晚起
【诗文】：
卧听冬冬衙鼓声，起迟睡足长心情。
华簪脱后头虽白，堆案抛来眼校明。
闲上篮舆乘兴出，醉回花舫信风行。
明朝更濯尘缨去，闻道松江水最清。
【注释】：
【出处】：
全唐诗
卧听冬冬衙鼓声，起迟睡足长心情。
华簪脱后头虽白，堆案抛来眼校明。
闲上篮舆乘兴出，醉回花舫信风行。
明朝更濯尘缨去，闻道松江水最清。
【注释】：
【出处】：
全唐诗
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