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c age data
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  “c age data”译为未确定词的双语例句
     , and integrated with the archeology, the ~(14)C age data in loess plateau and the cultural remains found in DXF-N profile, the results showed that the 4 sheet erosion-deposit events were recorded in DXF-N profile in 11500 a B.P. ~ 11000 a B.P.
     结合考古地层学、黄土高原已有的文化层~(14)C年代数据和在DXF-N剖面发现的文化遗物,确定出这四个面流侵蚀沉积事件分别发生在11500~11000 a B.P.
短句来源
     In the light of distribution and lithological features of the sediment, and 14C age data this paper consider the sediment to be Middle Pleislocene series mudflow sediment and not to be glacial and outwash sediment.
     根据堆积的展布和岩性特征,以及~(14)C年代测定资料认为,这一套堆积物属第四系中更新统泥石流堆积,并非冰川和冰水堆积物。
短句来源
     This paper presents many new data which were obtained from field observations during the past 10 years, of which related ~(14)C age data are vcry valuable. Based on the above data, the Quaternary glacial epoch of the area can be divided into the following from early to later: l) Yajiageng glacial stage of the Middle Pleistocene; 2) Early Hailuogou glacial stage of the Late Plcistocene;
     本文着重介绍了作者近10年来在该区考察中取得的大量新资料,特别是~(14)C年代资料,在此基础上对该区第四纪冰期划分出8期(次)冰期(冰进、间冰阶段),并进行了对比。
短句来源
     By Neutron Activation Analysis(NAA) method, chemical elements contents of Xihu lake core in Antarctic were gained, coupled with the result of 14 C age data, It was found that , in recent 2000 years, elements contents of lake core were changed with environmental change.
     用中子活化分析技术分析了南极西湖岩芯 (长 1 4 6 cm)中地球化学元素含量 ,结合14 C定年技术 ,发现近 2 0 0 0年来 ,地球化学元素在沉积物中的含量变化与沉积环境密切相关 ,尤其是稀土元素总量ΣREE出现峰值时 ,往往反映了温暖湿润的气候条件 .
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  相似匹配句对
     Data were grouped by age.
     其中髋部骨折组 16 2人 ,平均年龄5 3 4岁 ;
短句来源
     DATA
     数据
短句来源
     ON OPTIMIZATION OF MEASURING DATA OF ~(14)C AGE
     ~(14)C年代测量数据的优化
短句来源
     Research on Image Data Compression at the Age of the Network
     网络时代图像数据压缩研究
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     The age of the staffs is a public and objective data.
     人的年龄是一个公开显示的客观数据。
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  c age data
The atmospheric14C concentration (Δ14C) at their growing ages were obtained from the14C age data.
      
On the basis of correlation analysis of our data to a14C age data set, INTCAL of CALIB (Stuiver), the growing ages of these Japan cedars were estimated (BC 1090-2375).
      


This fault is developed in a drill bole of Quaternary deposit. The character and the dip of this fault is similar to the solid rock fault in same hole. According to the determination of 14C age data, the loose deposit in this drill hole is formed in Late pleistocene, thus they are thought to be the produces in the same time or represent a renewal of an ancient fault in or after the Late Pleistocene. Based on the analysis and Comparision of the characters and the occurrence of other faults which distributed...

This fault is developed in a drill bole of Quaternary deposit. The character and the dip of this fault is similar to the solid rock fault in same hole. According to the determination of 14C age data, the loose deposit in this drill hole is formed in Late pleistocene, thus they are thought to be the produces in the same time or represent a renewal of an ancient fault in or after the Late Pleistocene. Based on the analysis and Comparision of the characters and the occurrence of other faults which distributed in drill holes or solid rock around this hole, the fault can be determined to be a new active fault of Epipleistocene, its strike is N55°-65°w, the dip of WS and inclination is 45-75°.

该断层是在钻孔内的第四系沉积层发现的,它与同一孔内基岩的断层倾角、性质雷同.据~(14)C测年鉴定,断层所在的沉积物的年代为晚更新世晚期。据此认为它们是同一时期的产物,或者是此前形成的断层,近期活动的结果。结合周围钻孔和邻近基岩露头断裂的分布、产状等特征的分析对比,确定了该断层的产状是走向N55~65°W倾向SW倾角45~75°,是一条晚更新世活动的断层.

Predecessors have done quite a lot of investigations and studies on genesis and era of widespread clayey-gravel in Guilin, and advanced many views such as glacial sediment. We prospected two profiles and mapped two artificial exposure profiles during the hydrogeologic reconnaissance on scale of 1:200 000. According to differential thermal, spectral, chemical and spore-pollen analyses of collected samples the sedimentary environment is shown to be damp and hot. In the light of distribution and lithological features...

Predecessors have done quite a lot of investigations and studies on genesis and era of widespread clayey-gravel in Guilin, and advanced many views such as glacial sediment. We prospected two profiles and mapped two artificial exposure profiles during the hydrogeologic reconnaissance on scale of 1:200 000. According to differential thermal, spectral, chemical and spore-pollen analyses of collected samples the sedimentary environment is shown to be damp and hot. In the light of distribution and lithological features of the sediment, and 14C age data this paper consider the sediment to be Middle Pleislocene series mudflow sediment and not to be glacial and outwash sediment.

对桂林一带分布较广的第四系亚粘土砾石层的成因和时代,前人做过不少工作,提出过诸如冰川堆积物等看法。我们在进行1:20万水文地质普查时,有针对性地勘探剖面和测制人工露头剖面各两条。根据采集样品的差热、光谱、化学和孢粉分析,说明它的沉积环境是湿热的。根据堆积的展布和岩性特征,以及~(14)C年代测定资料认为,这一套堆积物属第四系中更新统泥石流堆积,并非冰川和冰水堆积物。

There are many Quaternary glacial development stages in the Hengduan(Transverse) Mountains, southwestern China, and palaeoglacial remnants of this area are well developed. This paper presents many new data which were obtained from field observations during the past 10 years, of which related ~(14)C age data are vcry valuable. Based on the above data, the Quaternary glacial epoch of the area can be divided into the following from early to later: l) Yajiageng glacial stage of the Middle Pleistocene;...

There are many Quaternary glacial development stages in the Hengduan(Transverse) Mountains, southwestern China, and palaeoglacial remnants of this area are well developed. This paper presents many new data which were obtained from field observations during the past 10 years, of which related ~(14)C age data are vcry valuable. Based on the above data, the Quaternary glacial epoch of the area can be divided into the following from early to later: l) Yajiageng glacial stage of the Middle Pleistocene; 2) Early Hailuogou glacial stage of the Late Plcistocene; 3) Qingshiban interglacial stage of the Late Pleistocene; 4) Late Hailuogou glacial stage of the Late Pleistocene; 5) Zhituoda glacial advance of the Holocene; 6) Dayanwo glacial advance of the Holocene; 7) Hailuogou glacial advance of the Holocene and 8) Glacial advance of the 17th to 19th centuries.Two conclusions are drawn in the end of this paper: 1) Quaternary glaciers were developed first in the Qinghai-Xizang(Tibet)Plateau and its activity then progressively migrated toward the Hengduan Mountains area. This regional regularity corresponds to uplifting of the Qinghai-Xizang Plateau. 2) The southern boundary of the activity of Quaternary glaciers goes as far as north of latitude 26°N.

横断山区是我国第四纪冰川发育期次较多、古冰川遗迹也最多的地区之一。本文着重介绍了作者近10年来在该区考察中取得的大量新资料,特别是~(14)C年代资料,在此基础上对该区第四纪冰期划分出8期(次)冰期(冰进、间冰阶段),并进行了对比。作者认为该区冰川具有明显的区域性规律,其与青藏高原抬升有关;横断山区第四纪冰川活动范围可至北纬26°线以北。

 
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