tanlu 中文意思是什麼

tanlu 解釋
丹路
  1. 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
  2. Multiple rotation and amalgamation processes of dabie - tanlu - sulu orogen

    蘇魯造山帶復合旋轉拼貼作用
  3. Study on collision tectonics in the east asia : tanlu - shangtaer collision zone

    尚塔爾碰撞帶研究
  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. 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
  9. 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
  10. 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
  11. 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。
  12. While there is no distict evidence to prove the tanlu fault ' s noted deep and dynamic behavior within the lower crust or even on the upper mantle. thus there still exists a necessary to research and check the understanding about the boundary ' s location and the dynamic background

    作為一級構造單元分界線的紅河斷裂、怒江斷裂是超殼斷裂，而昌寧雙江斷裂顯示為低角度鏟式斷層，中下地殼無與之對應的速度異常，可能意味著該斷裂切割不深。
  13. 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。
  14. 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。
  15. Based on the analysis of distribution of upper jurassic and lower cretaceous strata and basin - controlled faults, tanlu fault zone strike slip to develop the three nw - trending grabens from north to south western to tanlu fault zone in late jurassic and early cretaceous, which are bohai graben, jiyang graben and luxinan graben. based on the analysis of regional geology, the basic tectonic pattern of bohai basin is the cenozoic basin pattern since early paleogene. the outline, structure, deposit characteristics and heat flow distributions show that the basin is pull - apart basin in cenozoic time. the tectonic evolution pattern can be reconstructed based on the analysis of cenozoic strata, deposit thickness, location and activity of basin - controlled faults in the different depresses in bohai basin. the characteristics of structure and depositment in this mesozoic and cenozoic time show that bohai basin is a mesozoic and cenozoic composite basin

    根據中生界上侏羅統和下白堊統地層和控盆斷裂分佈分析，中生代晚期晚侏羅早白堊世郯廬斷裂帶的左旋走滑平移導致郯廬斷裂帶以西自北向南發育了3個北西向斷塹系，即北部的渤海斷塹系中部的濟陽斷塹系和南部的魯西南斷塹系。從區域資料綜合分析，渤海灣盆地的基本格局是早第三紀以來的新生代盆地格局。渤海灣盆地的形態構造和沉積特徵及熱流值分佈表明該盆地在新生代為拉分盆地。
分享友人
分享到 Line

分享到臉書