海西基底 的英文怎麼說

中文拼音 [hǎixījīde]
海西基底 英文
hercynian basement
  • 西 : west
  • 底 : 底助詞（用在定語后, 表示定語和中心詞之間是領屬關系, 現在多寫作「的」）
  1. This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement, whose tectonic deformation and magma intrusion is fiercely, and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian, it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area, such as a - granite ' s stock, batholiths and diabase ' s dike. there are many fault depressions possible

    按照不同構造層，研究了各構造層的構造特徵：基底構造層：受早海西期構造作用的影響，與準噶爾洋盆俯沖閉合、而後陸-陸碰撞的區域擠壓構造作用有關，為一構造變形和巖漿侵入活動強烈的古生代褶皺基底。二疊系構造層：受中海西區域性伸展斷陷作用的影響，盆地及其周緣地區發育與伸展構造有關的構造-巖漿組合，如呈巖株、巖基狀侵位的a型花崗巖以及呈巖墻狀侵位的輝綠巖等。
  2. Erlian basin is a rift lacustrine basin developed on the hercynian geosyncline folded base in early cretaceous, is featured by simple sedimentary feature, depositional cycle, small lacustrine transgressive, dry climate, salinization lacustrine water and multi - and - near sources

    摘要二連盆地是在海西期地槽褶皺基底上發育起來的早白堊世斷陷湖泊群，具有湖盆湖浸規模較小、氣候條件乾燥、湖水咸化、沉積旋迴單一，多物源、近物源和粗碎屑等沉積特徵，以及發育巖性地層油氣藏為主的油氣分佈特點。
  3. With an area of 5300 km2, dongpu depression is located in the southwest of lin - qing depression, bohaiwan basin, bounded with lu - xi uplift by lan - liao fault in the east, with nei - huang uplift by chang - yuan fault in the west, with lan - kao heave by the north feng - qiu fault in the south, with xin country depression by ma - ling fault in the north, while spreading along nne defection, taking on the forms of being wide in the south, and narrow in the north. it is a rift fault depression basin with the characteristics of striking, with the basement being the paleozoic and mesozoic, and the capping beds being the cenozoic

    東濮凹陷位於渤海灣盆地臨清坳陷西南端，東側以蘭聊斷裂為界與魯西隆起為鄰，西側以長垣斷裂為界與內黃隆起相接，南以封丘北斷層為界與與蘭考凸起相鄰，北以馬陵斷層為界與與莘縣凹陷相望，是以古?中生界為基底，以新生界為蓋層，古近紀形成的拉分走滑?裂谷型箕狀斷陷盆地。
  4. Based upon the analysis of the data obtained during the survey, it can be concluded that : 1 ) the number of biomass of macrobenthos in the yellow sea and the east china sea in autuma is higher than that in spring, while the number of density of macrobenthos in autumn is lower than that in spring ; 2 ) the number of biomass of macrobenthos in the yellow sea is higher than that in the east china sea ; 3 ) the number of species in the yellow sea is lower than that in the east china sea ; 4 ) one of the characteristics of distribution of macrobenthos in the east china sea is that the species richness increased from the coastal waters to the offshore deep waters, from the north to the south. 5 ) the species composition in the deeper part occupied by the cold water mass of the yellow sea is more stable than that in the coastal part of the yellow sea in the late 40 ~ 50 years

    通過以上幾方面的分析，結果表明： 1 ）黃東海調查海域的秋季總生物量均高於春季，總棲息密度則低於早春季； 2 ）黃東海春季生物多樣性指數高於秋季； 3 ）南黃海、東海的水文特點顯著不同：東海底溫顯著高於南黃海底溫，東海底鹽亦高於南黃海底鹽； 4 ）南黃海春秋季生物量分佈無一致規律，東海春秋季生物量除長江口外基本上自近岸向外海逐步降低； 5 ）東海大陸架大型底棲動物的種類組成較南黃海更豐富； 6 ）東海大型底棲動物的分佈特點之一為：種類數由北向南、由近岸（西部）向外海（東部）逐漸增多； 7 ）在黃海冷水團控制的海域，其底棲動物種類組成較近岸海域穩定； 8 ）幾個生物多樣性指數各有側重，都能較好地反映底棲動物的分佈特點
  5. Started from benxi stage of late carboniferous, deposits of epiric sea were developed in this area along with the spreading of west - east direction and gentle depression of the basement

    從晚石炭世本溪期開始，由於東西向拉張，基底緩慢下沉，本區廣泛發育陸表海沉積。
  6. Concentrations of total suspended matter ( ctsm ) is unanimous with observational data and other scholars " researching results. the distribution of ctsm is higher along coast than other areas there is a tongue - like zone with high ctsm from north to southeast. the transport simulation result reveals that sm can spread to the okinawa trough for enough sea water mixing in winter. but in summer. sm can not traverse the big water barrier of kushino for different circulation character. this difference is probably related to the shifting n - s monsoon

    懸浮體輸送表明，在冬季，懸浮體除了在陸架上發生擴散外，由於海水的強烈混合作用和環流的季節性變化，部分中、底層懸浮體可擴散至沖繩海槽甚至西太平洋;在夏季，由於海水層化及夏季環流特徵，懸浮體基本不能穿越黑潮這一水障，這一差異可能是由於季風和不同環流特徵所引起的。
  7. And in the valley, betharam, and bethnimrah, and succoth, and zaphon, the rest of the kingdom of sihon king of heshbon, jordan and his border, even unto the edge of the sea of chinnereth on the other side jordan eastward

    還有在谷中的伯亞蘭、伯寧拉、疏割、撒分，就是希實本王西宏國中的餘地，以約旦河作疆界，直到基尼烈海的底端，都在約旦河東。
  8. Bachu arch is a large back - thrust uplift. tectonic evolution of its large boundary fault fracture have relation with oil / gas distribution involuntarily. its large boundary fault fracture is basement rift formed in late hercynian period and strongly actived in late himalayan period. oil / gas distribution of bachu - markit have relation with fault interspace distribution. so, this paper also discussed interspace distribution and movement stage of fault

    巴楚隆起是一個大型背沖斷隆，其邊界大斷裂的形成演化自然關繫到本區的油氣分佈，隆起的邊界大斷裂多是海西晚期形成的基底斷裂，后在喜山期強烈活動，兼具壓扭走滑性質。
  9. The marine benthic communities in the waters around kau sai chau were not of special conservation concern, and the intertidal zone was basically natural and typical

    在?西洲附近水域的海洋底棲群落並不具特殊保育價值，其潮間帶生境基本上是天然及典型的。
  10. The exhibition centre has five exhibition areas, introducing the hong kong international airport and its related infrastructure projects, including the lantau link, the airport railway, the western harbour crossing, the north lantau expressway, travel route 3, the western kowloon expressway, the west kowloon reclamation, the central and wanchai reclamation, and the tung chung development

    展覽中心設有5個展區，介紹香港國際機場和相關的龐大基建工程，包括：青嶼干線、機場鐵路、西區海底隧道、北大嶼山快速公路、三號干線、西九龍快速公路、西九龍填海計劃、中環及灣仔填海工程和東涌發展計劃。
  11. Line b : start at 8 : 30am at the gate of wanlvyuan hainan tropical wildlife park & botanical garden tropical ecological international airport mangrove swamp civilized ecological villages viewing the underseawater villages relics on the beachside centuries - years - old banyan oyster - cultivating farm back to haikou & disperse at the gate of wanlvyuan

    早8 : 30萬綠園出發西海岸帶狀公園海南熱帶野生動植物園（午餐）車覽熱帶生態機場海底紅樹林文明生態村百年參天樹岸觀海底村莊祖孫牽手榕生蠔養殖基地車覽瓊州大橋萬綠園散團。
  12. Line b : start at 8 : 30am at the gate of wanlvyuan hainan tropical wildlife park & botanical garden < lunch > tropical ecological international airport mangrove swamp civilized ecological villages viewing the underseawater villages relics on the beachside centuries - years - old banyan oyster - cultivating farm back to haikou & disperse at the gate of wanlvyuan

    早8 : 30萬綠園出發西海岸帶狀公園海南熱帶野生動植物園（午餐）車覽熱帶生態機場海底紅樹林文明生態村百年參天樹岸觀海底村莊祖孫牽手榕生蠔養殖基地車覽瓊州大橋萬綠園散團。
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