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coastal area of east zhejiang
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  浙东沿海
     Research on numerical modeling of "9711" typhoon wave field in coastal area of East Zhejiang
     浙东沿海“9711”台风波浪场数值模拟研究
短句来源
     A Tentative Discussion on the Geochemical Characters and Tectonic Setting of Alkali-rich Granites in the Coastal Area of East Zhejiang
     浙东沿海富碱花岗岩地球化学特征及其构造环境探讨
短句来源
     THE DISCOVERY OF UPPER PROTEROZOIC STRATUM ALONG THE COASTAL AREA OF EAST ZHEJIANG AND ITS SIGNIFICANCE
     浙东沿海新元古代地层的发现及其意义
短句来源
     The discovery of upper Proterozoic stratum provides important information for studying basic tectonics along the coastal area of east Zhejiang.
     从而为研究浙东沿海基底构造提供了重要而可靠的窗口。
短句来源
     Through total analysis of wave field,it illustrates that SWAN model can rationally reflect the wave field in coastal area of East Zhejiang.
     通过综合分述模型计算的波浪场,说明SWAN模型能够合理地反映浙东沿海的波浪场。
短句来源
  “coastal area of east zhejiang”译为未确定词的双语例句
     Calculation on the Pore Water Pressure Caused by Pile Sinking in the Coastal Area of East Zhejiang Province
     浙东沿海地区沉桩引起的孔隙水压力的计算
短句来源
     The distribution of"9711"typhoon wave field in the coastal area of East Zhejiang was calculated through SWAN model. The observed data from Dachen,Nanji and Pibamen three oceanographic stations in Zhejiang was verified.
     使用SWAN模型计算浙尔沿海海域在“9711”台风下的波浪场分布,并采用矩形网格,对浙江省内的大陈、南麂、琵琶门3个海洋站的实测资料进行验证。
短句来源
  相似匹配句对
     THE DISCOVERY OF UPPER PROTEROZOIC STRATUM ALONG THE COASTAL AREA OF EAST ZHEJIANG AND ITS SIGNIFICANCE
     浙东沿海新元古代地层的发现及其意义
短句来源
     Research into Gukuang's Whereabouts in the East Area of Zhejiang
     顾况浙东行踪考略
短句来源
     Discussion on the Development of the Coastal Area in the East Guangdong
     粤东沿海地区的区域发展
短句来源
     Research on numerical modeling of "9711" typhoon wave field in coastal area of East Zhejiang
     浙东沿海“9711”台风波浪场数值模拟研究
短句来源
     EAST CHINA AREA
     非物质文化遗产——我们的精神家园 华东地区
短句来源
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There is a large-scale alkali-richintrusive rock zone, with an NNE striking in linear distribution, in the coastal area of east Zhejiang. It is composed of alkali-feldspar granites and alkaline granites. The alkali-rich intrusive rocks are characterized by Si-high (SiO_2>76%), alkali-rich(Na_2O+K_2O>8.2%), Al-low (Al_2O_3<12.5%), Ca-and Mg-poor (CaO<0.4%,MgO<0.20%) and concentrations of Rb, Th(U),Nb (Ta), Zr, Zn,Ga, etc. The chondrite-normalized REE patterns exhibit a gently right-dipping V-type curve...

There is a large-scale alkali-richintrusive rock zone, with an NNE striking in linear distribution, in the coastal area of east Zhejiang. It is composed of alkali-feldspar granites and alkaline granites. The alkali-rich intrusive rocks are characterized by Si-high (SiO_2>76%), alkali-rich(Na_2O+K_2O>8.2%), Al-low (Al_2O_3<12.5%), Ca-and Mg-poor (CaO<0.4%,MgO<0.20%) and concentrations of Rb, Th(U),Nb (Ta), Zr, Zn,Ga, etc. The chondrite-normalized REE patterns exhibit a gently right-dipping V-type curve with a severe depletion in Eu. The characters arc essentially identical with those of alkaline granite in Kuiqi, Fujian and similar to those of the A-type granite in the achlan folded zone of southeast Australia. The, above studies indicate that the alkali-rich granite zone was formed as a result of the magmatic evolution at the late stage of the Yanshanian movement, controlled by a regional deep fracture, that is to say, its formation may be attributed to the upward intrusion of deep-source alkali-rich magma during the tension of the deep fracture on active continental margin.

在浙东沿海地区存在一条北北东向线型展布的、规模可观的富碱侵入岩带,岩带由碱长花岗岩和碱性花岗岩组成。其岩石地球化学特点是高硅(SiO2>76%)、富碱(N_2O+K_2O>8.2%)、低铝(Al_2O_3<12.5%)、贫钙镁(CaO<0.4%、MgO<0.2%)、富集Rb、Th(U)、Nb(Ta)、Zr、Zn和Ga等元素;稀土元素模式曲线具缓右倾“V”字形,铕亏损强烈。上述地球化学特征与福建魁歧碱性花岗岩基本一致并类似澳大利亚东南Lachlan褶皱带A型花岗岩。研究表明,该富碱花岗岩带是燕山晚期岩浆演化后期产物,受区域深断裂控制,即可能是处于活动大陆边缘的深断裂在拉张条件下由深源富碱岩浆上侵而成。

Micropaleobotanical fossil which had been found in upper Proterozoic of some strata in China and upper Riphian as well as Vendian system is Russian and Siberia platforms, was first discovered in Cawang formation(J3c ) of upper Jurassic or Guantou formation(K1g ) of lower Cretaceous sedimentary strata near Fenglin town at Yongjia county along the reaches of east Zhejiang Mesozoic volcanic areas. Based on the standard fossil, the stratum should helong to upper Proterozoic. The discovery of upper...

Micropaleobotanical fossil which had been found in upper Proterozoic of some strata in China and upper Riphian as well as Vendian system is Russian and Siberia platforms, was first discovered in Cawang formation(J3c ) of upper Jurassic or Guantou formation(K1g ) of lower Cretaceous sedimentary strata near Fenglin town at Yongjia county along the reaches of east Zhejiang Mesozoic volcanic areas. Based on the standard fossil, the stratum should helong to upper Proterozoic. The discovery of upper Proterozoic stratum provides important information for studying basic tectonics along the coastal area of east Zhejiang.

在浙东沿海大片中生代火山岩覆盖区的永嘉县枫林镇附近、地层时代原定为上侏罗统茶湾组(J3c)或下白垩统馆头组(K1g)的一套沉积地层中,首次发现较为丰富的、曾产于中国某些地区新元古界和俄罗斯陆台与西伯利亚陆台上里菲及文德系中的微古植物化石。据此.该地层时代应属于新元古代。从而为研究浙东沿海基底构造提供了重要而可靠的窗口。

During the reign of Jiaqing in the Min g Dynasty,the Japanese monk Ceyan Zhouliang entered the Ming Dynasty twi ce,which shows some policies made by the imperial govern ment in the Ming Dynasty for the trade with Japan,the disasters caused by J apanese pirates in the coastal areas of East Zhejiang and the ban on mariti me trade with foreign countries in th e Ming Dynasty,from which people can know something about the politics,economy,military and cul tural environment in Zhoushan at...

During the reign of Jiaqing in the Min g Dynasty,the Japanese monk Ceyan Zhouliang entered the Ming Dynasty twi ce,which shows some policies made by the imperial govern ment in the Ming Dynasty for the trade with Japan,the disasters caused by J apanese pirates in the coastal areas of East Zhejiang and the ban on mariti me trade with foreign countries in th e Ming Dynasty,from which people can know something about the politics,economy,military and cul tural environment in Zhoushan at that time.

明嘉靖年间日僧策彦周良两次渡海入明朝贡的经历,证见了明朝廷对日勘合贸易的某些政策,以及浙东沿海倭患和海禁情状。对此,人们可以从中了解当时舟山的政治、经济、军事和文化环境状况之一二。

 
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