1) late middle Pleistocene
中更新世晚期
1.
After the research of sedimentology,geomorphology and chronology in the Sanduizi-Wudongde reach,we come to the conclusion that the geomorphic feature of the lower reaches of the Jinsha River was formed in the late middle Pleistocene.
中更新世晚期,古金沙江曾在金坪子河段发生堵江,使得金坪子河段成为金沙江发育的局部侵蚀基准点,并影响着三堆子-乌东德河段的河流下切速率。
2) Middle-late Late Pleistocene
晚更新世中晚期
1.
A Review of the Study of Environmental Changes and Extinction of the Mammuthus-Colelodonta Fauna during the Middle-late Late Pleistocene in NE China
我国东北地区晚更新世中晚期环境变化与猛犸象—披毛犀动物群绝灭研究综述
4) Lianhua Cave
中更新世晚期-晚更新世早期
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) 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。
补充资料：更新世
| 更新世(约距今164万年前～约距今1万年前) Pleistocene Epoch 第四纪的第一个世，约开始于164万年前，结束于约1万年前。更新世时形成的地层称更新统，位于上新统之上 、全新统之下。1839年，英国C.莱伊尔把巴黎盆地含软体动物化石70％为现生种的地层称为更新世地层。更新统下限的确定见晚第三纪。 |
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参考词条