1) Hongguleleng Formation
洪古勒楞组
1.
The Late Devonian Hongguleleng Formation, widespread in northern Xinjiang, consists mainly of thin-bedded marl, bioclastic packstone, volcaniclastics, siliceous rock, siltstone clastics and limestones.
小嘴贝类腕足动物Planovatirostrum形态奇特,在我国,目前仅在新疆北部和布克赛尔蒙古族自治县和什托洛盖镇北10余公里处七里沟剖面洪古勒楞组中段底部层位中发现,化石大致呈簇状密集或花斑状分布。
2.
At its type locality,the Hongguleleng Formation has been identified as the deposits of the latest Late Devonian and regarded for a long time as the highest unit predominated with marine beds of the Famennian age in northwestern margin of Junggar Basin,as well as in the whole northern Xinjiang.
标准地点的洪古勒楞组长期以来一直被认为是准噶尔盆地西北缘，乃至整个新疆北部以海相为主的层位上最高的晚泥盆世晚期的沉积。
2) Nailenggele
奈楞格勒
1.
The gold polymetallic deposit of Nailenggele in west Tianshan in Xinjiang is located the area of the main keel of Boluohuoluo mountain,and it is the cryothermal gold polymetallic deposit.
新疆西天山地区奈楞格勒金多金属矿位于博罗霍洛山主脊一带,属热液型金多金属矿。
3) Hanguletag formation
巷古勒塔格组
1.
Nodular limestones of Hanguletag formation in the Kuruktag are part of a type of warty sedimentary sequence.
新疆库鲁克塔格地区巷古勒塔格组发育瘤状灰岩,是一种深水沉积序列。
4) Wangjialeng Formation
王家楞组
1.
Owing to the Wangjialeng Formation established in 1: 200000 Foping quadrangle was considered to be an anticlinal structure here, this formation used to treat as lowest horizon of Devonian System in Feng (Fengxian County) Tai (Taibai county ) regions Continue to use so far,.
1：20万佛平幅区调建立的王家楞组由于原认为该处为一背斜构造，一直被当做凤太地区泥盆系最低层位沿用至今。
5) palaeoflood
古洪水
1.
Although palaeoflood research has only been practiced for 50 years,it is important for forecasting possibility and severity of floods.
尽管古洪水的研究最多只有50年左右的历史,但是利用全新世古洪水研究来补充洪水频率计算的资料,对预测洪水发生的可能性和严重程度具有重要的意义,所以古洪水的研究发展比较迅速。
2.
Palaeoflood information is based on the recognition and correct judgement to its carrier-slackwater deposits of palaeoflood.
古洪水信息的取得依赖于对其信息的载体──古洪水平流沉积作出准确的识别和判定，其判定的标志之一是粒度分析。
3.
To obtain a palaeoflood discharge based on the pinch outs of its slackwater deposits,the palaeoflood channel cross section area is required.
根据中国四大江河（ 长江、黄河、海河、淮河） 古洪水研究的成果，提出了在冲淤变化型河床上进行古洪水行洪断面面积估算的方法，即将估算的断面面积分为三个部分：现代均衡断面面积、古洪水均衡断面面积和次洪水冲刷断面面积。
6) paleoflood
古洪水
1.
Design Flood Calculation of the Qin River Based on Paleoflood Method;
古洪水研究方法在沁河设计洪水计算中的应用
2.
Through investigation of paleoflood deposits on the Xiaolangdi reach of the Yellow River, and by use of the field mark system for deposits judgement , identified are three types of the paleoflood deposits with four characteristics,and four geomorphologic types for the valid kind of slack water deposit.
通过分析古洪水沉积的环境及应用沉积物识别的野外特征指标体系 ,指出黄河小浪底河段的古洪水沉积分为 3种类型 ,具有 4个特点 ,其中赋存古洪水平流沉积的地貌类型有 4种 。
3.
Based on the paleoflood study for the Yangtze,Yellow,Hai and Huai Rivers in China, a comparison is made of the design flood with and without paleoflood data,and the analysis of rationality of design flood with paleofloods is also discussed in this paper.
根据长江、黄河、海河及淮河的部分河段上古洪水研究工作所取得的成果 ,按水利水电工程实际洪水计算的方法 ,将有古洪水资料的洪水频率计算成果与无古洪水资料的设计洪水成果相比较 ,从参数区域协调平衡、相同控制面积下设计洪水成果等的合理性检查方面论述加入古洪水资料后其设计洪水成果的合理
补充资料：翅楞楞
1.形容分散，分离。
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