1)tempestite风暴岩
1.Researches on tempestites of the Member 2 and Member 3 of Lower Permian Xiashihezi Formation in Daniudi Gasfield,Ordos Basin;鄂尔多斯盆地大牛地气田下二叠统下石盒子组盒2及盒3段风暴岩研究
2.Discovery of distal calcareous tempestites of upper ordovician age from Tianzhu, Gansu;甘肃天祝斜壕地区上奥陶统远源钙质风暴岩的发现
3.Discovery of late Early Triassic tempestite in Tongren area,Qinghai,China and its significance青海同仁地区早三叠世晚期风暴岩的发现及其意义
英文短句/例句
1.A Review of the Study of Tempestite with Special Reference to Significance of Tempestite in Xingwen County风暴岩研究述评兼论兴文风暴岩研究的意义
2.Characteristics of the Sandy Tempestites in the Middle-Upper Silurian of Lower Yangzi District and The Sequence of the Sandy Tempestites in the Shizikou, Chao County下扬子地区中上志留统砂质风暴岩特征和巢县狮子口剖面风暴岩序列
3.Discovery of Middle-Upper Cambrian Tempestites and Its Significance in Huangshi,Eastern Hubei Province鄂东黄石地区中上寒武统风暴岩的发现及意义
4.Features and Their Siginificance for the Tempestite of Neoproterozoic Shiwangzhuang Formation in South Shandong Province鲁南新元古界石旺庄组风暴岩特征及其意义
5.Discovery of distal calcareous tempestites of upper ordovician age from Tianzhu, Gansu甘肃天祝斜壕地区上奥陶统远源钙质风暴岩的发现
6.TYPES, CHARACTERISTICS AND GEOLOGIC SIGNIFICANCE OF THE DEVONIAN PYROCLASTIC TEMPESTITES IN EAST AND WEST JUNGGAR, XINJIANG东、西准噶尔泥盆系火山碎屑风暴岩类型、特征及其地质意义
7.This paper describes characteristic succession of dolomitic limestone tempestites from Middle-Upper Cambrian in Huangshi, eastern Hubei Province.鄂东黄石地区中上寒武统中下部发育一套典型的白云质风暴岩。
8.TEMPESTITE AND ITS PALAEOGEOGRAPHICAL SIGNIFICANCE OF DEVONIAN IN JINGYUAN AND JINGTAI COUNTIES,GANSU PROVINCE甘肃靖远─景泰泥盆系湖相风暴岩及其古地理意义
9.Tempestite of Akeshake Formation in Awulale Area,Western Tianshan and its significance西天山阿吾拉勒一带石炭系阿克沙克组风暴岩及其意义
10.Composite Deposits of Beach Bar and Tempestite in the Upper Fourth Member of Shahejie Formation in the Central Uplift Belt of Huimin Depression惠民凹陷中央隆起带沙四上亚段滩坝与风暴岩组合沉积
11.Discovery of late Early Triassic tempestite in Tongren area,Qinghai,China and its significance青海同仁地区早三叠世晚期风暴岩的发现及其意义
12.The discovery of the tempestites is of great significance to restructure the palaeogeography of Middle-Late Cambrian in Huangshi, eastern Hubei Province.该风暴岩的发现对重建鄂东黄石地区中晚寒武世古地理及区域地层对比具有重要意义。
13.This paper describes unique succession of calcareous tempestite from the Early Cambrian Qingxudong Formation, northeastern Guizhou Province.在黔东北铜仁－江口地区下寒武统清虚洞组下部发育一套特征典型、序列特殊的钙质风暴岩。
14.The storm cast the little rowboat on the rocks.风暴把这条小划艇抛到岩石上。
15.The billow of the atlantic dash high on the rock during a storm.暴风雨时,大西洋的巨浪冲撞岩石掀得很高很高。
16.The billows of the Atlantic dash high on the rocks during a storm暴风雨时,大西洋的巨浪冲撞岩石掀得很高很高
17.The lee of the rock gave them protection against the storm.岩石的遮掩使他们得以免受暴风雨袭击。
18.a raging tempest [sea]狂暴的暴风雨[海]
相关短句/例句
tempestites风暴岩
1.The Sedimentary Characteristics of the Tempestites in Zhenlongchang Formation, Zhaertaishan Group in Guyang Area,Inner Mongolia;内蒙古固阳渣尔泰山群增隆昌组风暴岩沉积特征
2.The Upper Devonian Xikuangshan Formation in Shilong, Liantang,Guiyang county,southeastern Hunan Province consists of limestones,dolomites,dolomitized limestones and lime dolomites of platform facies,in which typical tempestites develop.该组下部发育典型的风暴岩沉积。
3.Thetempestites of Paleogene in Huimin sag was discussed based on cores,rock thin section,granularity analysis and log data.利用钻井取心、薄片鉴定、粒度分析及测井解释等资料和手段,对惠民凹陷古近系风暴岩进行研究。
3)tempestite facies风暴岩相
4)tempestite deposits风暴沉积岩
5)Cale-windstormite钙质风暴岩
6)tempestite turbidite风暴浊积岩
延伸阅读
风暴岩 在风暴影响下在海洋和水盆地中形成的沉积岩。过去所称的浪成浊积岩实属风暴岩。风暴岩是一种密度流沉积，但常含很多风浪破坏下伏的正常天气沉积物所产生的撕裂片或内碎屑，还有被破坏的生物碎屑等。海洋中飓风等风暴可掀起涌浪，造成大片海面升高，海水流速增大，波浪传播加深；近岸的风暴潮常比正常高潮高出数米，潮差可比一般的大潮差大一倍多；波浪传播的深度常达几十米以上，远远超过好天气的正常浪基面的深度,甚至还导致近200米深的外陆棚的底流。风暴潮退潮可产生向海密度流，携有陆棚边缘的沉积物质，至潮下或陆棚上形成粒级递变层或在浅处形成发育丘状洼状等交错层理等的沉积层。 风暴作用特点为不但有高速流动，还有强的往复运动，方向时常改变，或有旋卷，而能量则在不太长时间内很快衰减。所以，风暴作用常将底部细物质簸出，常使风暴流形成密度流，在风暴衰减期迅速沉积。早期风暴作用对下伏沉积有侵蚀作用，形成侵蚀基底面，有冲蚀和侵蚀坑，形成充填构造。同时还可挖掘出浅埋藏物质，尤其生物体，使用底部物质混合，并形成混杂的生物组合。底部的大和重的个体生物在风暴作用中还可聚集成滞留层。常见的风暴岩如风暴介壳岩，含大部分破碎和少量完整的介壳，形成介壳灰岩，介壳砂岩，介壳粉砂岩等。多腕足类，双壳类，软体动物和海百合茎等化石，常具混杂的特征。组成的岩层厚几毫米到几厘米，或达十多米，常呈透镜状、口袋状。多位于侵蚀硬底上。常有寒武系的层内钙质砾岩，或称砾屑灰岩，竹叶状灰岩等。其刚性扁平内碎屑常呈杂乱状或涡卷状排列，无一定方位，表明受强烈振荡水流影响。 参考书目 G. Einsele & A. Seilacher eds,Cyclic and EventStratification,Part Ⅱ, Springer-Verlag, Berlin,1982.
