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晚更新世

n.epipleistocene
网络Late Pleistocene; Epipleistocene; Pieistocene

晚更新世

晚更新世

英-汉网络释义

晚更新世

Late Pleistocene

晚更新世（Late Pleistocene）也称上更新世，年代测定为126000年（±5000年）至10000年，是第四纪中更新世的最后阶段， …

Epipleistocene

石油英语词汇(E3)_英语行业_英文阅读网 ... epiplatform 地台浅部；边缘地台 Epipleistocene 晚更新世 Epiproterozoic 上元古代 ...

Pieistocene

　出现年代：晚更新世(Pieistocene)

2

Some early-formed faults or fault segments continued to be active, while the others have become inactive.

某些断层或断层段继续活动；另一些先存断层在晚更新世以来不再活动；

3

Since the Late Pleistocene, the tectonic regime has changed to strike slip and reverse faulting one.

晚更新世以来，构造体制转化为走滑 —逆冲机制。

4

Many geological evidences show however that larger lake and high lake levels once existed in this area during the Late Pleistocene .

但多次考察结果揭示晚更新世时期存在着大湖和高湖面的地质证据。

5

6

Since the late Pleistocene, the two faults haven' been active .

晚更新世以来，两断层均没有活动迹象。

7

This led the research team to conclude an extraterrestrial impact wiped out many of the inhabitants of the Late Pleistocene.

从而导致研究小组作出结论，认为来自地球外的冲击力摧毁了许多晚更新世的栖息动物。

8

Since late Pleistocene, this segment was relatively inactive on the whole.

晚更新世以来，该段基本上处于比较稳定的状态。

9

This lake lasted about two millions years and vanished in the Late Pleistocene.

大同 -阳原古湖历时二面馀万年，至晚更新世末消亡。

10

Xiashu loess is a kind of special eolian deposits in the late quaternary , originating from middle and lower reaches of the Yangtze River .

下蜀土是我国区域性分布的一种特殊的风尘沉积性土壤，形成于第四纪晚更新世，普遍发育于长江中下游地区。

11

Kuqi underlying fault is a late epipleistocene last stage active fault . And the newest active time was about 14 , 000 years apart from now.

库齐隐伏断层是一条晚更新世末期的活动断层，最新的活动时代为距今 1.4万年左右。

12

The highest terrace was formed in the Late Pleistocene.

最早的第三级阶地在晚更新世已经形成。

13

High-resolution paleoceanographic study of the Okinawa Trough Since the late Pleistocene

冲绳海槽晚更新世以来高分辨率古海洋学研究进展

14

We believe that the Shenzhen fracture zone had no perceptible activities since late Pleistocene by fault profiles and fault material ;

通过对断裂带地层剖面和断层物质研究发现，断裂带晚更新世以来没有明显活动迹象；

15

The micro-structural characteristics of the Late Pleistocene loess and its environmental meaning in Xianyang City

咸阳市区晚更新世黄土微结构特征及其环境意义

16

Late Pleistocene Sedimentary Stratigraphic Structure and Its Implication in the Central and Western Areas of Southern Yellow Sea

南黄海中西部晚更新世沉积地层结构及其意义

17

Spore-pollen records of environmental change on south coast plain of Laizhou Bay since the Late Pleistocene

莱州湾南岸滨海平原晚更新世以来古环境演变的孢粉记录

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Tectonic Deformation of China Continent and Its Adjacent Regions since Late Pleistocene Inferred from Active Fault Movement Data

用活断层资料分析中国大陆及其邻区晚更新世以来的构造应变特征

19

Sedimentary Characteristics of Weihe Palaeochannel Since Late Pleistocene and Their Control to Modern Salt-Water Intrusion

晚更新世以来潍河古河道沉积及其对现代咸水入侵的控制

20

Late Pleistocene Marine Dinoflagellate from Dongying Depression, Shandong Province

山东东营凹陷晚更新世海相沟鞭藻类

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