holocene
Of, belonging to, or denoting the Holocene Epoch.
全新世的属于或表示全新世的
The Holocene Epoch or its system of deposits.
全新世时期或该时期的沉积系统
Dodos are flightless birds from the late Holocene.
渡渡鸟是全新世晚期不会飞翔的鸟类。
This saphire deposit is occurred in the Holocene alluvium.
矿床赋存于全新统冲积层。
The priciple of cyclic sedimentation applies to deposits dating from earliest Paleozoic time to the Holocene.
旋回沉积原理适用于始于最早的古生代迄至全新世的沉积物。
The principle of cyclic sedimentation applies to deposits dating from earliest Paleozoic time to the Holocene.
旋回沉积原理适用于始于最早的古生代迄至全新世的沉积物。
It lived in Eurasia, from Ireland to east of Lake Baikal, during the Late Pleistocene and early Holocene.
它生活在欧亚大陆，从爱尔兰到东部的贝加尔湖，在晚更新世与全新世早期。
The vegetation was dominated by steppe or sparse steppe in the early Holocene,corresponding to a warm and dry climate.
全新世早期气候温凉略干，为草原型植被或稀疏草原型植被；
Holocene Recent geological epoch following Pleistocene, began ca. 10,000 years ago.
全新世在更新世之后的最近地质学纪元，大约在10,000年以前开始。
Some scientists proposed that the Holocene optimum of the East Asian monsoon was asynchronous among different regions.
另一方面则可能暗示了不同的沉积序列、测年材料之间难以进行精细的对比。
M. (2002) Holocene rock uplift and subsidence in coastal area of Taiwan: AGU 2002 Fall meeting.
中国地质学会九十一年年会暨学术研讨会摘要集。
The features and formation of calcites reveal that dry and hot climate has prevailed in Yuanmou Basin since Holocene.
次生方解石的形成过程及特筇下反映了自全新世发来元谋盆地主要处于干热气候环境中。
Abstract : This article has a brief review on Holocene climate changes in Mongolia.
摘要 ： 简要地回顾了蒙古全新世气候变化研究。
The main sediments of Holocene sections are clay and sand soil with mini sand layers in North Taklimakan desert.
全新世以来塔克拉玛干北部（以下简称塔干北）主要沉积物组成为亚粘质土、细砂夹杂着粉砂。
So, it provides many new ponderations and enlightenments in understanding Holocene stratum and basement tectonics of the Hebei Plain.
因此，它对全面认识河北平原的全新世地层和新构造运动形迹会有许多新的启示。
Elevations of sulfurous layers in acid sulfate soils: What do they indicate about sea levels during the Holocene in eastern Australia?
酸性硫酸盐土壤中含硫磺土层的高度:对澳大利亚东部全新世时期的海平面能说明什么?
Stratigraphic division and establishment of a formation for the Holocene stratotype section in the coastal plain of the Bohai Bay.
渤海湾滨海平原全新统层型剖面地层划分与建组
The studies of Mongolian Holocene climate changes mainly focused on the records of tree-rings, eolian sediments and lacustrine sediments.
蒙古全新世气候变化研究侧重于对树轮、风成沉积和湖泊沉积物的研究。
According to the characteristics of pollen and spore assemblages, lithology and nanofossils, the climate in the middle Holocene was warm and humid.
根据第三阶段的孢粉组合特征、岩性特征以及微体化石可知，全新世中期的气候比较适宜，气候温暖湿润。
This previously undiscovered species is a cestoid parasite, up to 30 centimetres long and weighing up to 70 grams from the late Holocene.
这种之前没有被发现的物种来是全新世晚期，是一种绦虫，超过30厘米长和70克重。
Palynology which provides numerous evidences plays an important role and makes great contributions to the research on Holocene environment changes.
孢粉学在全球环境演变研究中提供了大量证据，发挥了重大作用，成果显著。
Exemplified by Jingpohu Holocene volcanic rocks, this paper has discussed the relationship between melt structure and volcanic eruptive mechanism.
本文以镜泊湖全新世火山为例，讨论了熔体结构和某些火山喷发机制的关系。
The semi-buried pluvial-alluvial terrace in front of the mountain and the Holocene pluvial-alluvial fan compose sloping plain in front of the mountain.
多项证据显示新构造运动趋势：在中更新世以间歇性构造抬升为主，自晚更新世以来却变成间歇性下沉或稳定。
In regard to the climate of North China in Holocene, a series of problem, such as the law of spatio-temporal variety, demand to be resolved.
就华北地区全新世气候变化研究而言，还存在一系列需要解决的问题，如气候时空变化规律性问题等。
These rapid climate changes occurred in the last glacial stage, but also in the Holocene and the middle and early Pleistocene.
不仅见于末次冰期，也发生在全新世和早、中更新世。
The Holocene climate is arid and changes between hot dry and cool dry,which is mainly controlled by global longitude wind and cyclone.
塔干北气候变化受全球径向环流影响较大，纬向环流影响较小。
Wuguan marine erosion physiognomy has important geognosy significance in the study of structural movement and the changes in sea level in period of Holocene Epoch.
对于研究全新世构造运动、全新世海平面变化等具有重要的科研、科普价值。
The 14C dating data of cheniers should be used with great prudence. And it is also not suitable to use the chenier as an exact mark of the Holocene sea level change.
贝壳堤贝壳~(14)C测年资料应当慎用,也不宜把古贝壳堤看成全新世海平面变化的确切标志。
During the late Holocene(3kaBP after),the coastline moved rapidly and the wide seashore plain were formed as the Yellow River captured the Huaihe River.
晚全新世(3kaBP以来)因黄河夺淮,海岸东迁迅速,形成广袤的滨海平原.
The climate change of North China in Holocene include three periods and eight stages.The unsteady mechanism of climate change is needed to be studied ulteriorly.
华北地区全新世气候变化大体可以分为三个时期八个阶段，这种气候变化不稳定性机制尚待进一步研究。
But high TOC and C/N ratio during MIS 5.1, 3.3 to 3.2 and the Holocene reflect that the terrigenous organic matter input increased during interglacial periods.
2期和全新世高的有机碳含量和C/N比值反映间冰期陆源有机物质输入量的增加.
The shallow layer nature gas at the extrance of Hangzhou Gulf mainly existed in the stratums between Holocene epoch and Pleistocene epoch of the 4th Era.
杭州湾地区浅层天然气主要赋存于第四纪全新世和晚更新世地层中。
From the LGM(18 ka BP) to the Holocene transgression(10 ka BP),great changes took place in world climate, including the paleo monsoon activity which occured in the Eastern Asia.
从距今18000年的最后冰期最盛时期到距今10000年开始的全新世海侵,全球气侯发生过急剧的变化。位于亚洲东部的古季风活动也经历了盛衰变化。
The Quaternary is subdivided into the Pleistocene epoch and the Holocene epoch, and is characterized by major cyclical changes of climate on a global scale.
被划分成更新世和全新世。第四纪的特徵是气候在全球规模上有大的周期变化。
The duration of Holocene Optimum defined as a postglacial interval of the most equable climate with warm temperatures and abundant rainfall has not been beyond debate.
在不同地点适宜期的起止时间、表现特征总存在一些差异，一方面可能体现了不同的局地地形、植被、水文条件等对区域水热条件的不同反馈；
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.
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。
Wang Z., Chen Z., Chen J., Wei Z., 2007. Seismic framework to interpret the Holocene morphological evolution of the Changjiang River mouth, China. Geomorphology, in press.
赵宝成，王张华，陈中原，太湖平原碟形洼地沉积记录的距今8000年以来的植被、气候与地貌演变,古地理学报（已接受）
Quaternary (Neogene) The most recent period of the Cenozoic era from about two million years ago to the present day and composed of the Pleistocene and Holocene epochs.
第四纪（新第三纪）：新生代最近的一段时期。它从大约2百万年到现在。由更新世和全新世组成。
Holocene(Recent) The present epoch in the geological time scale, being the second epoch of the Quaternary period, dating from the end of the last glaciation, about 10000 years ago, to the present day.
全新世：在地质学上指第四纪的第二阶段的整个时期，它终止于最后一个冰川期，距今大约10000年。
During the Banpo man time or in the Middle Holocene, 5000~6000 Bp, the climate within the modern glaciation best fitted vegetation and the intrusion of some sub-tropic trees was postulated to have taken place.
古土壤代表间冰期夏季风盛行的湿热气候，植被比较繁盛；黄土代表冰期冬季风盛行的干冷气候，植被凋凌。
Yao Tandong, Shi Yafeng.Climatic changes of Holocene reflected in the ice core from Dunde, Qilian Mountains.In: Shi Yafeng, Kong Zhaochen eds.The Climates and Environments of Holocene Megathermal in China.Beijing: China Ocean Press,1992.
姚檀栋,施雅风。祁连山敦德冰芯记录的全新世气候变化。见:施雅风主编,孔昭宸副主编。中国全新世大暖期气候与环境。北京:海洋出版社,1992。
Based on the sedimentary system of Poyang Lake basin from Holocene,the sedimentary system of the margin of Poyang Lake basin presents asymmetry,and shows cyclicity in vertival series.
以全新世以来鄱阳湖盆地沉积体系为基础,发现在鄱阳湖盆地边缘沉积体系呈现不对称性,垂向系列上呈现旋回性。
Based on the sedimentary system of Poyang Lake basin from Holocene, the sedimentary system of the margin of Poyang Lake basin presents asymmetry, and shows cyclicity in vertival series.
摘要以全新世以来鄱阳湖盆地沉积体系为基础，发现在鄱阳湖盆地边缘沉积体系呈现不对称性，垂向系列上呈现旋回性。
These are coastal swamp stage, developing lagoon stage, bay stage, coastal lowland stage and desalinated lagoon stage, which are closely related to the Holocene regional sea level change and coastal environmental evolution.
即滨海泥沼阶段、泻湖阶段、海湾阶段、滨海低地阶段和淡化泻湖阶段。 这五个阶段与本地区全新世以来的海面变化及环境变迁紧密相关。
The planimetric positions of these faults were consistent with the fault positions in the map of Tertiary geologic structure, which indicate that some fault motions were from the Pleistocene to Holocene epoch.
这些断层的平面位置与基底或第三纪地质构造图中的断层位置一致,表明有些断层活动贯穿了更新世并延续到全新世,这些勘探成果对渤海西部断层活动性的鉴定具有重要意义。
Synthesize analyse according to the field Research and the material of bore holes, in holocene period, the Yong Ding Rivar flooded into the Xiao Qing River, only limited between the Xiao Qing River and Dashi River.
根据野外调查和钻孔资料综合分析,永定河在全新世期间曾泛流进入小清河,范围仅限于小清河与大石河之间。
The results have shown that Tangshan seismogenic fault is a NW dipping dextral strike slip Quaternary contemporaneous fault,which offsets the Holocene(Q 4),late Pleistocene (Q 3),middle Pleistocene(Q 2) and early Pleitocene(Q 1) strata.
结果表明：唐山地震断层是一条倾向NW的右旋走滑第四纪同生断裂，它错断了全新统（Q4）、晚更新统（Q3）、中更新统（Q2）和早更新统（Q1）地层。
The earthquake occured on the NNW trending tectonic belt which lie on the east of the Pamirs that new construct activity is intensive, most of faults in the tectonic belt is dextral strike-slip Holocene deep faults.
地震发生在新构造活动强烈的帕米尔高原东部北北西构造带上,该构造带的断裂性质多为右旋走滑的全新世活动深断裂。
Abstract: On the basis of field investigation and laboratory analysis, it was found that there were three lay-ers of aeolian sand in Huahai Section, a Holocene lacustrine sediments.
通过野外调查和室内分析，发现在花海剖面全新世出现了三次风成沙沉积，并对其原因进行了初步分析。
According to analysis, beachrock is mabe up of terringenous clastic and bioclast, the cement are mainly aragonite and high Mg calcite. 14C dating data of beachrock samples show that Lianyungang beachrock formed in the Early Holocene.
经岩石样品及簿片、扫描电镜、~(14)C同位素等分析测定,海滩岩主要由陆源碎屑和生物碎屑组成,胶结物为文石和高镁方解石.