郯 的英文怎麼說

中文拼音 [tán]
郯 英文
名詞1. （古國名） tan, a state in the zhou dynasty2. （姓氏） a surname
  1. Hefei basin that is located on the southern fringe of the north china plate and by the side of tan - lu fault zone is a mesozoic cenozoic continental basin

    合肥盆地為一中、新生代陸相盆地，位於華北板塊南緣、郯廬斷裂帶西側近旁側。
  2. Meso - cenozoic evolution of the tanlu fault and formation and distribution of petroliferous basins

    郯廬斷裂帶中新生代演化與含油氣盆地形成分佈綜述
  3. Due to the west north direction subduction, fast collapse ( delamination ) may take place and the mantle plume emerged in ludong, in addition, owing to the subduction of pacific plate under eurasian, there appeared left - lateral advection and extension for tan - lu faults ( named as yishu fault in shandong ), and together with the collapse of yanshanian orogenic belts, all induced the crustal extension in shandong

    由於太平洋板塊對歐亞板塊的俯沖（ nw向） ，魯東地區巖石圈發生了快速拆沉減薄作用，同時魯東地區也可能會出現地幔柱的活動；另外，在太平洋板塊俯沖作用影響下，郯廬斷裂（山東稱沂沭斷裂）帶發生了大型左行走滑剪切和拉張活動。
  4. Recent activity of chihe segment of tanlu fault zone

    郯廬斷裂帶池河段的新活動
  5. The tanlu fault zone and gold ore metallogenesis

    郯廬斷裂與金礦成礦
  6. Bouguer gravity study of middle section of tanlu fault

    應用布格重力異常研究郯廬斷裂構造
  7. Liaohe basin is a part of tanlu rifting system, and it belongs to continental rift basin

    遼河盆地是郯廬斷裂系的組成部分，屬大陸裂谷盆地。
  8. Structural features and cenozoic evolution of the tan - lu fault zone in the laizhou bay, bohai sea

    萊州灣地區郯廬斷裂帶的構造特徵及其新生代演化
  9. Progress in the study of the southern segment of the tanlu fault and a discussion of the nature of the fault

    郯廬斷裂南段研究進展與斷裂性質討論
  10. Characteristics of tertiary period basalt of the middle tanlu fault belt and the relationship of corundum

    郯廬斷裂帶中段第三紀玄武巖特徵及與剛玉形成的關系
  11. The tectonic character of tanlu fault and the relation between tlf and hydrocarbon accumulation in bozhong sag

    郯廬斷裂在渤中凹陷的構造特徵與油氣成藏的關系
  12. 7. the dabie orogenic belt is of transformation and superposition character. its new superimpose

    Ne向郯廬斷裂系的大型平移作用疊加在原來印支期消減帶之上，產生新的俯沖。
  13. The first part mainly surveys the regime construction of tancheng county of shandong province before 1949

    第一部分，主要是簡要回顧山東省郯城縣1949年以前政權建設的概況。
  14. Firstly, it summarizes the transitional characteristics of the grassroot regime in tancheng county from 1949 to 1954

    首先簡要總結了1949至1954年郯城縣基層政權的過渡性特點。
  15. The third part mainly observes the regulating improvement and gradual finalization of the grassroot regime in the county

    第三部分，主要考察郯城縣的基層政權在調整中繼續完善和逐漸定型的基本情況。
  16. The biological features of flowering were studied in 26 superior individual male ginkgo biloba trees selected from 5050 male trees in taian and tancheng of shandong province

    對從泰安和郯城共5050株銀杏雄株中篩選出的26個優良單株的開花生物學特性進行了研究。
  17. In a word, the stress field variation since mesozoic can be divided into five periods such as indosinian epoch, early yanshan epoch ( j3 - k1 ), end of yanshan epoch, eogene, neogene and quaternary, it is mainly affected by the active pattern of tanlu large fault

    綜合研究認為，本區自中生代以來的應力場變化可分為印支期、早燕山期（ j3 - k1 ） 、燕山末期、早第三紀、晚第三紀及第四紀五個階段，應力場的變化主要受郯廬大斷裂活動方式的影響。
  18. The depositional character of zhuxiang formation in the basin reads as follows : a series of nne alluvial fan were formed along the fault. the half - deep lake to deep lake faces appeared by west side of the fault, towards the west the saucer lake faces, shore deposit and flood plain face appeared in proper order. the depositional center of lower cretaceous was formed in eastern part of the basin, and the depositional depth was pinch - out and thinning out from the east to the west

    盆地內下白堊統朱巷組沉積特徵表現為：沿郯廬斷裂帶呈北北東向廣泛發育了沖積扇體系，從近斷裂帶西側出現的半深湖-深湖相，向西依次為濱淺湖相到泛濫平原相的規律性分佈，沉積厚度由東向西尖滅、超覆，構成了明顯的東斷西超的盆地構造格局，表明下白堊統的沉積中心依然位於盆地東部。
  19. By researching geology condition and geology background, discourse thinks that tanlu rupture is mine - leading structure, the greater ne - orientation ruptures are ore - proportioning structure, sn - orientation ruptures are ore - containing structure in mouru ore belt

    結合膠東區域地質條件和地質背景，論文提出郯廬斷裂為牟乳金礦帶的導礦構造，一系列北東向的大型斷裂是配礦構造，而牟乳地區的北北東向斷裂只是容礦斷裂。
  20. The electrical resistivity tomography survey was conducted to detect the active faults along the tanlu fault zone in weifang, shandong province

    摘要在城市活斷層調查中，利用電阻率二維層析成像測量方法，對郯廬斷裂帶山東濰坊段的地震活斷層進行了探測試驗，取得了較理想的勘探效果。
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