川澄 的英文怎麼說
中文拼音 [chuāndèng]
川澄
英文
kawazumi-
Satsuki exhibition, satsuki gardening class and more events such as the edo traditional craft workshop ( including charged experience ) are scheduled during the festival period. visitors may enjoy tour around other gardens on the special stamp rally project where you can access by the toei subway oedo line. those on the list are hama - rikyu onshi gardens, koishikawa korakuen gardens and kiyosumi gardens
除江戶傳統工藝角（有可交納成本費體驗的活動）以外，同時從舊芝離宮恩賜庭園開始通過都營大江戶線連接的濱離宮恩賜庭園、小石川后樂園、清澄庭園等景點處，還可蓋上不同地方的精美郵戳。On the toei subway oedo line, a convenient route is via fukagawa shiryokan - dori. 15 - minute walk from the no. 3 exit of kiba sta
都營地鐵大江戶線清澄白河站a3出口步行13分鐘經由深川資料館大道便捷。Alkali basite, which came from upper mantle or lower crust, invaded through those structure, which not only bring cu et al mineralizing elements, but also the most important is that thermal energy. it cycled the formation water ( yinmin fonnation and luoxue formation ), and form alkali - rich, middle - high temperature and salinity fluid mixed with alkali - rich magmatic water. there were high rate of percolation and well voidage in the contact zone between yinmin purple stratum and yinmin rubblerocks, which is in favor of the transposition and mineralization of minerogenetic fluids
因此，總結東川稀礦山式銅礦成礦模式為沉積（ fe 、 cu ） ?熱液疊加（ cu ）改造：晉寧-澄江期，小江深大斷裂發生走滑運動，在東川礦區造成右行旋扭及其派生構造，形成「 z 」字形落因破碎帶，同時來自深源（下地殼或上地幔）堿基性巖漿侵入，不僅帶來了大量cu等成礦物質，更重要的是提供了熱源，促使地層水（落雪組白雲巖和因民組紫色層）循環，與富堿（ na和k ）巖漿水混合，形成富堿中高溫高鹽度流體。D ) the invasion of jinningian - chengjiangian alkali basite were unambiguous, the distribution of those rocks form " z " in shape, which similar with luoyin fracture zone and the distribution of copper deposit. it shows that copper deposits were controlled by discordogenic fault and its derived sub - structure, and there are relationship between copper deposit and jinningian - chengjiangian alkali basite. e ) most of minerogenetic age of copper deposit, which located in kunyang rift valley, belongs to jinningian - chengjiangian ( between 900 - 650ma ), similar with the time limit of breaking - up of rodinia
東川礦區晉寧-澄江期堿基性巖侵入活動明顯，常作為因民組復雜角礫巖膠結物和巖脈（體）產出，多分佈於深大斷裂及其派生的次級構造附近，明顯受南北向小江深大斷裂走滑運動引起的右行旋扭及其派生構造控制，與「落因破碎帶」和「銅礦分佈」較吻合，均為「 z 」字形。It indicates there are close relationship between the forming of copper deposit in kunyang rift valley and the breaking - up of rodinia
表明東川礦區銅礦形成與深大斷裂及其派生次級構造和晉寧?澄江期堿基性巖侵入活動關系密切； 5Even before that, i was told that there was a temple called mirokuji in front of our house ( near 3 - chome, morishita, kiyosubashi - dori ), and people came to the temple to get a permit to make a visit to ise shrine
此外，從前在家前面（清澄大道、立川1丁目附近）的彌勒寺里，聽說前往參拜伊勢的人們還會得到發行的通行證。分享友人