intermediate adj. 中间的,居间的。 The intermediate class (船的)特别三等。 An intermediate compound 中间化合物;中间体。 n. 中间物;中间分子,中间人;【化学】中间体;期中考试;中间试验。 vi. 起调解作用;起媒介作用 (between)。 Intermediate culture 补植。 Intermediate elements 中间分子。 adv. -ly 在中间。 -ness, -diacy n. 调解。
rock n. 1.岩,岩石,磐石,岩壁;卵石;〔常 pl.〕〔美口〕石子儿;暗礁,岩礁。 2.〔the R-〕直布罗陀 (Gibraltar) 的别名。 3.〔比喻〕靠山,护符。 4.〔比喻〕隐藏的危险[困难],祸根。 5.=rock cake, rock candy. 6.〔英国〕硬糖果;硬干酪。 7.〔美国〕用来投掷的石头;〔美俚〕金刚钻,宝石(等);〔美俚〕一块钱;〔pl.〕钱。 8. 〔俚语〕碡〔一种结晶状可卡因〕。 a needle of rock ?岩。 a sunken rock 暗礁。 Rocks ahead! 前面有暗礁!危险! an almond rock 杏仁味硬糖。 as firm as a rock=like a rock 安如磐石,坚定不移,屹然不动。 built [founded] on rock 建立在岩石上的;基础坚固的。 driven on the rock 触礁。 on the rocks 触礁;搁浅;手头拮据;进退两难;〔美俚〕分文没有的,破了产的。 run [strike] upon the rocks=thrown on the rock 触礁。 see rocks ahead 看到前途的暗礁,看到前途的危险。 split on a rock 在暗礁上撞得粉碎;完全破灭[失败]。 the Rock of Ages 【宗教】永久的磐石〔原为基督教会一首赞美诗的题目,现指耶稣和基督教〕。 vt. 1.摇,摇动,使振动。 2.【采】摇选。 3.摇引…入睡;抚慰。 4.使感动,打动;使震动,使震惊。 He rocked back and forth in his chair. 他坐在椅子上前前后后地摇。 rock the baby to sleep 摇婴儿入睡。 a rocking gait 摇摇摆摆的步态。 vi. 1.摇动,动摇;振动;摇摆;蹒跚。 2.感动;震动。 n. 1.摇;动摇。 2.摇摆,摇摆舞曲。 n. -ism 摇滚乐。 n. 〔古语〕(手纺用)卷线杆。
In the jinshajiang suture zone , it lasted only a span of 9 ma from the start of subduction ( marked by the eruption of andesitic magmas and intrusion of intermediate rock of iag type at about 227 ma ) to the end of subduction , consumption of oce Iv期: 45ma以来,高原快速抬升;断裂系活化,产生大规模走滑活动;岩体或被断层切割、迁移,或抬升剥蚀。 ivi : 45 25mi ,岩体和整个青藏高原一起呈周期性的、脉动式抬升。
The results indicate : ( 1 ) the distribution of magmatic rocks shows the feature that in the middle and western part of the study area basic igneous rocks dominate , and in the middle - eastern part intermediate rocks are predominant , while in the southeastern part acid ones are developed . ( 2 ) in the area west to the shiwandashan basin , intermediate magmatites were controlled by deep ne - striking and nw - striking faults , especially at the conjunction site of these two group faults , magmatic activity was strong ; and its tectonic background can be attributed to extensional continental rift 其中,在十万大山盆地以西地区的偏基性岩浆活动受北东和北西向深断裂控制明显,尤其以此两组断裂交汇处的岩浆活动强烈,盆地构造背景属大陆伸展裂谷环境;在十万大山盆地以东地区为偏酸性岩浆活动,主要受东吴运动形成的钦防造山带的控制,属大陆边缘造山带或岛弧造山带环境。
A ree partition simulation suggests that the tianzhushan intermediate rocks can be generated by partial melting , in coupling with fractional crystallization , of dioritic gneiss which is similar in chemical compositions to the mafic rocks in the lower crust in north dabie ; partial melting of intermediate grey gneiss which is similar in chemical compositions to the middle crust in north dabie can generate the tianzhushan felsic rocks Ree配分的定量模拟计算结果表明,与基性下地壳相似的北大别基性闪长质片麻岩部分熔融并经过结晶分异能够形成与天柱山中性岩类似的稀土元素组成,而与中性地壳相似的北大别中性灰色片麻岩部分熔融能够形成与天柱山花岗岩类似的稀土元素组成。
Ree partition simulation suggests that the tianzhushan intermediate rocks can be generated by partial melting , in coupling with fractional crystallization , of dioritic gneiss which is similar in chemical compositions to the mafic rocks in the lower crust in north dabie ; partial melting of intermediate grey gneiss which is similar in chemical compositions to the middle crust in north dabie can generate the tianzhushan felsic rocks Ree配分的定量模拟计算结果表明,与基性下地壳相似的北大别基性闪长质片麻岩部分熔融并经过结晶分异能够形成与天柱山中性岩类似的稀土元素组成,而与中性地壳相似的北大别中性灰色片麻岩部分熔融能够形成与天柱山花岗岩类似的稀土元素组成。