The results of rupture landform investigation indicate that this fault is one of weak active faults in Holocene, its average vertical slip rate is 0.5~0.6mm/a. On Jun. 15, 1975, Liuba M6.2 earthquake in Kangding occurred on the fault. The macro-epicenter located at Shuobu-Moda, Liuba county. The direction of long axis of meizoseismal area is same as that of Yunongxi fault trend. The occurrence of the earthquake is resulted from the newest activity of the fault.
断错地貌研究结果表明，该断裂为一条全新世弱活动断裂，平均垂直滑动速率为0.5~0.6mm/a左右。1975年1月15日康定六巴6.2级地震发生於该断裂上，宏观震中位置位於六巴乡溯布－莫达村附近，极震区长轴方向与玉农希断裂走向一致，是该断裂最新活动的表现。
From the view of position, the youngest Maanshan and Laoguipo volcanoe s in Holocene Epoch are just located in the place that S wave passes, and Daying shan volcano is nearby.
从地表位置看，腾冲最年青的全新世的马鞍山和老龟坡火山就在S波掠过范围内，打鹰山火山也在近旁。
Neogene can be divided into one second-order sequences with Holocene and 5 third-order sequences in Huanghekou depression.
在黄河口凹陷新近系与全新系划分出1个二级层序、其中新近系划分出5个三级层序。
By analysing most experiment data, the relation between compressive modulus of Holocene (Q 24) sedimentary clay and standard penetration test blowcount has been set up.
本文简略论述了新近沉积土的一般特征，通过分析研究大量的试验数据，确定出了新近沉积粘性土的压缩模量ES与标准贯入试验锤击数 N值的关
Brought forward and reasoned the forming mechanism of Maowusu sandy land. Based on the analysis of the development of Holocene rivers and related loess and windsandy geomorphology, the paper put forward the forming mechanism of Maowusu sandy land as follows: while the climate became dry, the exterior channels extended backwardly and cut through the remained lake system of ancient Hetao lake. This resulted in the rapid discharge of underground water. The vegetation living on this water resource was destroyed completely. Then the sand began to form.
对毛乌素沙地的形成机制进行了新的探索基于对过渡地带全新世河流及其相关的黄土和风沙地貌发育、土地利用变化等分析，提出毛乌素沙地的形成机制：在气候变干的同时，外流河谷溯源延伸，切穿了长城以北河套古湖残遗湖系，使地表地下水迅速外泄，原靠湖系水资源维系的生长在河套古湖湖滨沙堤形成的沙地上的非地带植被的生存条件被彻底摧毁，而起沙。
Two geomagnetism pole drifts during the Holocene are recorded in northern part of the BSMA, occurring at 2800~3100 aBP and 7500~8200 aBP respectively.
北部记录着全新世期间发生的两次地磁极漂移，分别发生于2800~3100 aBP和7500~8200 aBP。
In the Holocene, the general climate in the source area was cool and dry and characterized by the plateau cold climate.
在全新世，黄河源区的气候总体凉干，属于高原的高寒气候。
The geochemical features of element associations can be used to indicate the locations in cores of the main paleoceanographic events which have happened since the last glacial maximum, such as Holocene/Pleistocene boundary event and loung Drgas event in the Okinawa Trough
显然，在物源和岩性均比较稳定的情况下，沉积物的元素组合可以作为环境变化的替代性指标用以进行古海洋学和过去环境变化的研究。
Soda salinity was mainly enriched in the sedimentation area of Holocene basin centrally of which was the serious disaster area of modern soil salin...
苏打盐份主要富集于全新世盆地的沉降区，沉降中心为现代土壤盐碱化的重灾区。
There are three parts: the part from the west of Gejiagou to northwest of Yamalikeshan mountain is latest mid Pleistocene epoch activity; the part from the east of Gejiagou to Tiechanggou is late Pleistocene and the east of Tiechanggou is Holocene activity.
断裂活动时代大体分为3段：葛家沟以西至雅玛里克山西北麓，为中更新世晚期活动；葛家沟以东到铁厂沟，为晚更新世活动；铁厂沟以东为全新世活动。
14C dating of a sample taken from the section of Swan Lake at 70.5 cm below the surface gave an age of 4930±152 a, indicating that the section mainly formed in the Holocene, which is the same as the age of the stone implements found at Sogo Nur.
在进行地质环境调查过程中，在内蒙古额济纳旗苏泊淖尔Ⅰ级湖积阶地面上发现古人类遗存的石制品，包括石砧、石斧、石片、石核等，大致应属于全新世的遗存。
The mean thickness of the bands during the Holocene Optimum (265μm) ranges twice of that during the LGM (102μm), which indicates strong East Asian summer monsoon may be beneficial for the growth of the stalagmite.
全新世大暖期年纹层平均厚度(265μm)约为末次盛冰期(102μm)的2.5倍，说明在间冰期东亚季风增强时石笋沉积速率较大，冰期时则相反。
By means of magnetic susceptibility, Rb/Sr ratio and pollen analyses, the climate changes were divided into three periods during the midlate Holocene: from 52 ka BP to 42 ka BP, the temperature and precipitation were higher than present in this area, but the climate turned into cool and arid with fluctuations at the end of that time; 4220 ka BP was a coolarid period; a relatively warmwet period occurred after 20 ka BP.
沉积样品的磁化率、Rb/Sr比值和已有的孢粉分析结果反映的气候变化趋势基本上是同步的。52 ka BP以来屈家岭遗址附近区域气候变化可以分成3个阶段：52~42 ka BP期间，是较为温暖湿润的时期，水热条件好于现在，后期暖湿程度有波动性降低的趋势；42 ka BP开始气候暖湿程度明显下降，气候转向干凉；20 ka BP以来，本地区气候暖湿程度有所回升。
After complete regional analogue, it is discovered that the palaeoclimate and palaeoenvironment in Tontso is entirely comparative and consistent with the synchronous lakewater retreating of Zhaduixiong spits in Zabuye Lake basin, with palaeoclimate changes recorded by pollen in adjacent Zhabuye Lake, with Holocene palaeoclimate environment indicated by drilling-hole in Bangong Co, with palaeoclimate significance traced by δ〓O value in Qinghai Lake and Siling Co, with pollen- and diatom-inferred climatic change in Longmu Co and Sumxi Co, and with the palaeoclimate framework during the 5〓 Level Arid Extension Period of Quaternary arid center of Western China.
对比研究发现，洞错的古气候环境，与同期相邻的扎布耶湖湖水退缩遗迹和花粉记录的古气候变化、班戈湖钻孔所揭示的全新世古气候环境、色林错δ〓O值所揭示的气候意义、龙木—松西错的孢粉和硅藻提供的古气候古环境信息以及第四纪西部干旱中心在第5级干旱扩张期中的古气候格局，它们的气候环境变化总体上均有可对比性和一致性。
We studied variability in micromollusk abundance and diversity in the Yongshu reef lagoon in the late Holocene, and their relationship with the temperature record of the Northern Hemi- sphere, in order to document the micromollusk response to climatic variability on shorter timescales.
本文试图通过南海永暑礁泻湖微型软体动物丰度和分异度的研究及其与北半球温度异常的对比，来阐述微型软体动物对快速气候变化的响应。
The results show that the climate fluctuated in different stage during the Holocene, that is, the climate was cool and wet during 9455～8635 acal.
在拱王山狐狸房峰附近保存着典型的第四纪冰川遗迹，一些学者对此进
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。
The warmest and humidest period in Holocene, strong summer-wind and pedogenesis, similar climate with the Middle and Lower reach of Yangtze River currently, weakened sand storm and aeolian dust accumulation, strong leaching and argillic processes, the most suitable period was 6760～6520aB. P.; Late Holocene 3100～1500aB. P.
为全新世最温暖湿润期，夏季风强盛，气候类似长江中下游现代气候，风沙活动和风尘堆积减弱，成壤强烈，土壤淋溶和粘化作用较强，气候最适宜期为6760～6520aB.P。
Drainage systems incising late Pleistocene-Holocene alluvial fans record between 3m and 250m dextral offsets and show progressive displacement along the fault zone.
发育在晚更新世－全新世冲积扇中的水系记录了3~250m的右行错断和位移的累积。
These minerals are typical of iron meteorite. The iron meteorite occurred in Holocene sediments, so it landed in Holocene.
该区历史上没有陨石降落的记载，根据该铁陨石产出在第四系的全新世冲－洪积层中离地表3~4m的深度处，推断它的降落年代应是全新世。