Middle Pleistocene

The earliest differentiation in the complex is estimated to be approximately 200 000 years ago between S Yunnan region and East region during the later Middle Pleistocene .

大约是在200000年前滇南区群体与东部区群体最早发生分化，处于中更新世的晚期。

Since the Middle Pleistocene , with the evolution gradually to a coastal and shallow marine environment , distal upper reaches of the Yangtze River have deposited in the area .

总之，中更新世以来，在环境逐渐向滨、浅海演变的过程中，远源的长江上游物质已经在本区沉积。

Study on Time and Mode of Middle Pleistocene Transition

轨道周期转型时间及模式分析

Rapid changes in East Asia winter monsoon in early and Middle Pleistocene

早、中更新世东亚冬季风强度的快速变化

The third fold developed between late Early Pleistocene and early Middle Pleistocene .

早更新世晚期，中更新世初期，第三排褶皱开始形成。

At the end of Middle Pleistocene , the third terrace was formed ;

中更新世末，该区发生隆升，形成第三级阶地；

Its sedimentary time is around the late stage of Middle Pleistocene to Upper Pleistocene .

沉积时代为中更新世晚期至晚更新世。

This discovery has filled the gap in Middle Pleistocene fossils .

这一发现弥补了川西高原中更新世无断代化石的空白。

Middle Pleistocene high-resolution palynological sequences and climate changes in the northern South China Sea

在伊莫拉所做的空力套件更新中的一部分。南海北部更新世高分辨率孢粉序列与气候变化

The Environment Character Of Middle Pleistocene In The Area Of Dali Man Site In Shanxi Province , China

陕西大荔人遗址地区中更新世环境特征

Law of water infiltration of lower part of Middle Pleistocene loess in Luochuan of Shaanxi

陕西洛川中更新统下部黄土入渗规律研究

It is middle Pleistocene in age .

年代地层单位属中更新统。

The development of Benxi water cave started from the middle Pleistocene , about 400000 years ago .

本溪水洞的发育起始于中更新世，即约40万年前。

Magnetism stratigraphy of middle Pleistocene red clay in Xianlin area , Nanjing City

南京仙林地区中更新统红色粘土的磁性地层学特征

Pollen records and vegetation and climate changes in Heqing Basin , Yunnan Province since middle Pleistocene

云南鹤庆盆地中更新世以来的孢粉记录及其植被与气候变化

Environmental events and catastrophes from the end of early pleistocene to the early stage of middle pleistocene

上新世-更新世近海砂层早更新世末中更新世早期的环境事件与灾变

Middle Pleistocene ( strata 8 & 7 );

中更新统（层（8-7））；

The three circles of the warm-cold fluctuations in the Middle Pleistocene were recognized .

第1地点记录了中更新世三次明显的气候冷暖波动。

The Paleoenvironment Research on Loess Susceptibility and Particle Size Characteristics Since Middle Pleistocene in Ning Cheng County Inner Mongolia

内蒙古宁城中更新世以来黄土磁化率与粒度特征及古环境研究

In Middle Pleistocene Epoch , Taihu Lake Plain was a fluviolacustrine alternative sedimentary environment .

中更新世时期，太湖平原为河湖交替的沉积环境。

The middle Pleistocene loess has no collapsibility .

中更新统黄土一般不具有湿陷性。

The upper unconformity engenders the sediment absence of top middle Pleistocene to top upper Pleistocene .

上部不整合造成中更新统顶部至上更新统上部间的缺失。

Middle Pleistocene Revolution ( MPR ) that gave rise to the global climate changing , formation of Western Pacific Warm Pool ?

前后引起全球气候变化的中更新世革命（MPR）、西太平洋暖池的形成以及0.78MaB.P。

The middle Pleistocene loess is granule-floor cemented with skeleton touch space and no collapsibility .

中更新统黄土为不等粒基底胶结结构，存在骨架接触式孔隙，一般不具有湿陷性；

Middle Pleistocene strata : gravel layer ; sand , coarse sand interbedded with gravel layers ; gravel layers .

中更新世：砾石层；砂、粗砂与砾石层互层；砾石层。

The Kunlun-Yellow River Tectonic Movement is an intense tectonic movement at the turn from Early Pleistocene to Middle Pleistocene .

昆仑黄河运动是发生在早、中更新世之交的一次强烈的构造运动。

Alluvial facies of Middle Pleistocene dated at 190 ~ 220 ka BP , with warm-humid climate .

中更新统上部的冲洪积沉积（190~220KaBP），气候较暖湿等阶段。

Middle Pleistocene paleoecology , paleoclimatology and paleogeography of the western coast of POHAI Gulf

渤海湾西岸中更新世以来古生态、古气候、古地理

The characteristics of the red bounder clay , that formed in the middle pleistocene can 't be compared with those of the debris flow formed at present .

用现代泥石流堆积物特征与之直接对比，以论证其成因的方法是不可靠的。

These changes from 0.93 to 0.62 Ma recorded in eolian loess-paleosol sequences possibly respond to the world-wide middle Pleistocene climatic transition event .

这种变化可能是黄土高原风尘堆积对中更新世气候转型事件的响应。黄土高原岩石磁学记录的中更新世气候转型事件发生于0.93Ma，结束于0.62Ma。