冀北晚更新世地层划分为迁安组与马兰组。
The Upper Pleistocene in northern Hebei is divisible into the Qian an Formation and the Malan Formation.
其层位相当于丁付组下部，时代为晚更新世早期。
Its horizon is equivalent to the lower of the Dingcun Formation and its age is early Late Pleistocene.
延怀盆地晚更新世中晚期湖泊沉积反映了潮湿气候的特征。
The lake sediment of the middle and late time of late Pleistocene reflects a wet climatic characteristic of the Yanhuai basin.
杭州湾地区浅层天然气主要赋存于全新世和晚更新世地层中。
Shallow gas in the area of the Hangzhou Bay mainly exists in the Holocene and upper Pleistocene of Quaternary.
在晚更新世末期，中国陆架环境的最显著特点是寒冷而干燥。
In the last stage of the Late Pleistocene, the main features of the sedimentary environment in China continental shelf were cold and dry.
具体到中卫断裂带来说，就是指晚更新世以来新发育的断层。
With regard to the Zhongwei fault zone, it refers to the one which has developed since late Pleistocene.
中更新世与晚更新世早期的海进较弱，仅有海陆过渡相沉积。
The transgressions of Middle Pleistocene and the early Late Pleistocene were weak and represented by deposits of the transitional nature from Marine to continental facies...
中更新世与晚更新世早期的海进较弱，仅有海陆过渡相沉积。
The transgressions of Middle Pleistocene and the early Late Pleistocene were weak and represented by deposits of the transitional nature from Marine to continental facies only...
中更新世与晚更新世早期的海进较弱，仅有海陆过渡相沉积。
The transgressions of Middle Pleistocene and the early Late Pleistocene were weak and represented by deposits of the transitional nature from marine to continental facies only. The strongest tran…
这对于理解晚更新世地中海地区居民的祖先及其关系是重要的。
This relationship is an important one for understanding the ancestry and relations of the Levantine populations of the Upper 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。
Many geological evidences show however that larger lake and high lake levels once existed in this area during the Late Pleistocene.
对探槽揭露的断层分析表明，这些断层自晚更新世以来未发生新活动。
The data on test trenches reveal that these thrusts have had not any activity since the late Pleistocene.
晚更新世以来自然环境的变化直接影响着黄土高原国土资源的开发利用。
The change of the natural environment of the loess plateau has directly affected the development and utilization of the land resources in the loess plateau.
东段烟台-威海段为中更新世活动段，没有发现晚更新世地层错断现象。
The eastern Yantai-Weihai segment is a mid Pleistocene segment on which no late Pleistocene offset has been found.
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；
Some early-formed faults or fault segments continued to be active, while the others have become inactive.
造成晚更新世时期两岩芯沉积相的差异主要与断裂构造的升降运动有关。
The different sedimentary environment at late Pleistocene was mainly due to vertical motion of fault block.
进一步研究表明，西昆仑山地区西段中晚更新世至少经历了3次强烈的隆升。
Further study suggests that the western of the west Kunlun Mountains in the Mid-late Pleistocene has undergone at least 3 times strong upheaval.
野外考察重点考察在晚更新世黄土—古土壤序列及同时期不同岩性地层单位间的差异。
The excursion will focus on Late Pleistocene loess-palaeosol sequences in the area and the differentiation of coeval lithostratigraphic units.
泥石流沉积物作为晚更新世一种特殊沉积类型，是在特定的地质过程和地理环境中形成的。
As a special deposit type, debris flow deposit forms in specifically geological structure and geographical environment.
以上的研究为北京平原晚更新世晚期人地环境的重建和进行史前人类历史的研究提供依据。
These results provide evidences for the reconstruction of the geomorphic environment of Beijing plain during the Late Pleistocene and the study of prehistoric human history.
根据构造地貌与新构造特征，推算了晚更新世以来山东半岛北部沿海地区的构造抬升速率。
Based on the tectonic landforms and neotectonic characteristics, the uplift rates along northern Shandong Peninsula since late Quaternary was calculated.
通过对钻孔岩心和浅地层地震剖面的分析，恢复了辽东湾北部晚更新世中期以来的沉积环境。
The deposit environment in the north of Liaodong Bay since the medium-term of late Pleistocene is rebuilt by the analyses of the core and the seismic profile.
丁村人被确定为早期智人，文化时代为旧石器时代中期，所属地质时代则被定为晚更新世早期。
The fossil hominids were diagnosed as early Homo sapiens, with a cultural age of Middle Paleolithic, and geologic age of early Late Pleistocen.
在多处发现断层露头剖面，断层错断了晚更新世和全新世沉积物，反映出断层具有很新的活动性。
The sections ot several fault outcrops have been discovered, in which the sediments of Late Pleistocene and Recent have been dislocated by faults, showing the fracture of new activity.
晚更新世至全新世，抬升速度减缓，稳定时间增长，而且在总体抬升的背景上，出现了沉降运动。
The speed of uplift became slow, and the period of stability became long from Neopleistocene to Holocene epoch. There were descending movement on the uplift background in Holocene epoch.
表明自晚更新世以来该区气候在逐渐变干的总趋势的基础上，经历了多次明显的冷暖与干湿波动。
Based on the general trend of getting arid gradually, the climate in the region experienced several marked cold-warm and dry-humid fluctuations since Late Pleistocene.
结合孢粉分析结果，本文探讨了青海省西部地区通天河及布曲流域晚更新世早中期的古植被与古气候。
Based on the U-series dating and sporopollen analysis, this paper presents a discussion on the paleovegetation and paleoclimate of the Buqu Basin and its adjacent regions during the interval 88.
晚更新世晚期，至全新世以来，第二排褶皱与第三排褶皱一直在持续隆升，同时第四排褶皱也开始形成。
The second fold and the third fold had been uplifting from later period of late Pleistocene to Holocene, and the forth fold came into being at the same time.
青藏高原东北缘的中卫断裂带在晚更新世以来的左旋走滑运动中，先存的挤压逆掩、逆冲断裂带发生了分化。
The left-lateral strike-slip movement of the Zhongwei fault zone since late Pleistocene caused the differentiation of preexisting overthrust faults in the zone.
晚更新世以来的三次海平面升降变化造成了潍河下游地区海陆沉积环境交替，形成了巨厚的海陆交互相沉积层。
There were three times of sea-level fluctuation corresponding to the paleoclimate evolution, which had formed the sediments of alternative sea and river facies.
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