1) low limit of Quaternary
第四纪下限
2) lower limit of the Quaternary
第四系下限
1.
8 m contain 42 layers and are basically Quaternary in age (The lower limit of the Quaternary is at 761.
第四系下限初步定在761。
3) Quaternary
[英][kwə'tə:nəri] [美][kwə'tɝnərɪ]
第四纪
1.
Eco-environment change and influence factors in the Songnen plain since the Quaternary;
松嫩平原第四纪以来生态环境演化的影响因素
2.
Discovery of Quaternary potassic volcanic rocks and the establishment of Sailipu Formation in West Gangdis of Tibet, China;
冈底斯西段第四纪钾质火山岩的发现及赛利普组的建立
3.
Character of heavy minerals in Quaternary sediments in Yichang area and its relationship with cut-through of the Yangtze Three Gorges,China;
宜昌地区第四纪沉积物重矿物特征及其与三峡贯通的关系
4) late Quaternary
晚第四纪
1.
The exploration method of late Quaternary shallow biogenic gas reservoirs in Hangzhou Bay area.;
杭州湾地区晚第四纪浅层生物气藏勘探方法研究
2.
Environmental Changes of Late Quaternary in Source Rigion of The Huanghe River;
黄河源地区晚第四纪环境变迁
3.
Evolution of Paleovegetation and Paleoenvironment of Late Quaternary on Basis of Spore-pollen Analysis in Shanghai Region;
从孢粉推测上海地区晚第四纪以来的植被、环境演变
5) Quarternary
['kwɔ:tənəri]
第四纪
1.
Quarternary sediments in Shenyang are widely distributed with NE thin and SW thick,which basically is multilayered sand compound texture:the surface is a relatively thin clay,downward relatively thick and grading layers of fine medium grained sand,coarse grained sand,gravelly sand,and gravel.
沈阳市第四纪沉积物分布广泛，北东薄、南西厚。
2.
In the Tathang and Yan Mountains,incised and meandering valleys formed in Quarternary.
太行山、燕山山地中的深切曲流河谷形成于第四纪。
6) Quaternary period
第四纪
1.
Characteristic of Quaternary Period the earth crustal movement in Sanjiang Plain;
三江平原第四纪地壳运动特征
2.
Research on Debris Flow in South of Liaoning in Background of Quaternary Period;
辽南泥石流第四纪环境背景研究
补充资料：上限与下限
上限与下限
衰2利率和易变性时翔结构┌────┬───┬────┬───────┐│时间(年)│互换率│零息债券│远期利率易变性││ │(%) │利率(%) │ (%)(%) │├────┼───┼────┼───────┤│0。5 │3 .25 │3 .25 │ │├────┼───┼────┼───────┤│1 .0 │3.匆 │3 .53 │3 .75 15 │├────┼───┼────┼───────┤│1 .5 │3.印 │3 .73 │4.(y7 14 │├────┼───┼────┼───────┤│2 .0 │3 .88 │392 │446 14 │├────┼───┼────┼───────┤│2 .5 │4工 │4.佣 │4.麟13 │├────┼───┼────┼───────┤│3 .0 │4 .17 │4 .23 │4 .95 13 │├────┼───┼────┼───────┤│3 .5 │4 .31 │4 .39 │5 .26 12 │├────┼───┼────┼───────┤│4 .0 │4 .46 │4 .55 │5 .59 12 │├────┼───┼────┼───────┤│4 .5 │4.印 │4 .71 │5 .91 12 │├────┼───┼────┼───────┤│5 .0 │4 .75 │4 .87 │6 .25 12 │└────┴───┴────┴───────┘衰3上限和下限价格(所有标价为基点)┌──┬──┬──────┬──────┐│ │ │上限执行利率│下限执行利率│├──┼──┼──────┼──────┤│预付│如 │437一一 │肠137 222 ││价格│3yr │121 337一 │74 1582肠 ││ │5yr │413 191即31 │79 174引)3‘│└──┴──┴──────┴──────┘。298。中国金融大百科全书·下编9568178一116 5639，一一、?布一如如伽加分期支付价格892 53522343 129343巧1 91310 17514刃537302 1853 在计算上限收费价格时，很重要的一点是要注意应该与互换利率的执行价格相比较，而不是与短期通行利率(prev山ling short一~rate)相比较，否则可能会导致错误的结果。从这里所列示的时期结构(tenn slluc恤)看，短期利率为3.25%，而执行利率为5%的五年期上限看起来似乎严重损价(能U out ofthe伽ney)，因而1.91%的收费价格显得过于昂贵。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条