陸凹 的英文怎麼說

中文拼音 [liùāo]
陸凹 英文
depression of land
  • 陸 : 陸數詞（六的大寫） six （used for the numeral 六 on cheques, etc. to avoid mistakes or alterations）
  • 凹 : 凹名詞（凹陷的地方, 用於地名） low-lying area; depression （used in place names）
  1. Chagan sag is a secondary tectonic unit in chagandelesu depression, northeastern yingen - eji ' naqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate, with the character of erogenic belt. in working area and its adjacent area, the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly, intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase

    查干凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元，其盆地基底為古生代時期華北板塊、哈薩克斯坦板塊和塔里木板塊交接部位形成的陸緣或島弧褶皺帶，具有古生代造山帶的性質。研究區及鄰區印支期侵入巖形成於造山帶強烈擠壓陸內俯沖的構造環境；燕山早期侵入巖形成於由擠壓轉向拉伸、造山帶的增厚陸殼開始發生伸展垮塌的構造環境；早白堊世火山巖形成於造山期后進一步發生伸展垮塌的區域構造環境。
  2. Chagan fault depression is a secondary tectonic unit in chagandelesu subbasin, northeastern yingen - ejinaqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc with the character of erogenic belt at the connection region of north china plate, tarim plate and kazakstan plate

    查干德勒蘇凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元。其基底為古生代時期華北板塊、塔里木板塊和哈薩克斯坦板塊交接部位的陸緣或島弧褶皺帶，具有古生代造山帶的性質。
  3. In the 20th century a number of security features, ranging from embedded metal threads to intaglio printing, came into use

    到了20世紀，由內藏保安線以至凹版印刷技術等防偽方法也陸續面世。
  4. In east china sea shelf basin, the mesozoic relict sediments are distributed in some central - south areas, such as fuzhou sag, minjiang sag and yushan lower uplift

    摘要東海陸架盆地中生界主要分佈於盆地中南部的福州凹陷、閩江凹陷和漁山低隆起地區。
  5. The urogenital system of impressed tortoise manouria impressa

    凹甲陸龜的泌尿生殖系統
  6. The carbonate source rocks of middle - upper ordovician in tarim basin are widely distributed in different sedimentary environments at the same period such as platform margin slope, platform inner sag, continental shelf, abyssal basin, etc

    摘要塔里水盆地中上奧陶統碳酸鹽巖烴源巖在同一時期不同的沉積環境（臺緣斜坡、臺地內凹陷、陸棚、深海盆地等）中均有發育。
  7. A large, bowl - shaped depression in the surface of the land or ocean floor

    凹地，海盆在陸地或海底平面的一種大的，碗狀的凹地
  8. The mainland, not so very far off - - you could see clefts in the cliffs, white cottages, smoke going up - - wore an extraordinary look of calm, of sunny peace, as if wisdom and piety had descended upon the dwellers there

    內陸，不算太遠? ?竟能看到懸崖上的凹痕、白色小屋、炊煙裊裊升起? ?籠罩著一抹奇異的神色，充滿沉靜而陽光平和，好似智慧與虔敬降臨于那裡的居民。
  9. Yinggete - bagemaode metamorphic core complex belt with three - layer construction is put forward, which evolved from late jurassic to cretaceous. the extensional simple shear model of the chagan fault depression is established. the tectonic evolution and the dynamics character of chagan fault depression and its adjacent mesozoic - cenozoic basins are discussed : at the end of triassic continental orogeny increased crust thickness crust uplift and denudation were happened ; jurassic was a period of local partly extensional collapse of erogenic belt and cretaceous was a period of widely extensional collapse of postorogenic erogenic belt ; cenozoic was a period of the development of stable intracontinental depression with the character of long distant collision response and weaked compression flexure

    討論了查干凹陷及鄰區中-新生代盆地構造演化及其地球動力學特徵，三疊紀（印支期）為陸內造山作用與地殼增厚、隆升剝蝕階段；侏羅紀（燕山早期）為造山後造山帶的局部伸展垮塌階段；白堊紀（燕山晚期）為造山期后大規模伸展垮塌作用與伸展盆地的發育階段；新生代（喜山期）為遠距離碰撞效應與弱擠壓撓曲性質的穩定大陸內坳陷的發育階段。
  10. Analysis of petroleum geology, reservoir types and distribution in lujiapu depression indicates that : the forming and distribution of reservoirs had been controlled by source area, source - reservoir relationship, petrophysical characteristics, sedimentary facies and secondary structure, and oil is most abundant in reservoirs around hydrocarbon kitchen ; the upper member of jiufutang formation which was entrained or embedded in the main oil source layer has well developed reservoir and good petrophysical property and is the principle oil - bearing interval ; the mid - fan and fan delta front of nearshore submarine fan is the most favorite facies ; the steep slope of the depression mainly consists of structural reservoirs, the slope belt mainly consists of structural - lithologic and updip pinchout reservoirs, the depressed belt mainly consists of lenticular lithologic reservoirs

    摘要對陸家堡凹陷油藏形成的石油地質條件、已知油藏類型及分佈的分析認為：生油區、生儲配置關系、儲集物性、沉積相帶和二級構造帶控制了油藏的形成和展布，其中圍繞生油窪陷的油藏含油最豐富；夾持或嵌入主要生油層中，儲層發育、儲集物性又相對較好的九佛堂組上段是主要含油層段；近岸水下扇的扇中和扇三角洲前緣是最有利的相帶：凹陷的陡坡帶以構造油藏為主，斜坡帶以構造巖性及儲層上傾尖滅油藏為主，深陷帶主要為透鏡狀巖性油藏。
  11. To sum up the above analysis, we make sure that the pretertiary of haijiao uplift, yushan uplift and east flank in oujiang depression and the transitional zone between changjiang depression and xihu depression is a new prospect of time and space for hydrocarbon exploration in the shelf basin of the east china sea

    因此，海礁凸起、漁山凸起、甌江凹陷東側、長江凹陷與西湖凹陷之間以及浙閩隆褶帶的前第三系是東海陸架區油氣勘探的新領域。
  12. According to the differences of sedimentary facies and environment, the source rock are divided into four types such as lime - mud reef in platform margin, platform inner sag, deep - water flat slope or continental shelf, abyssal basin, the lime - mud reef type is distributed in platform margin of upper ordovician, the remained three types are widely distributed in cambrian - ordovician system

    根據沉積相帶與沉積環境的不同，可將烴源巖劃分為在不同沉積環境中的4種類型烴源巖；臺地邊緣灰泥丘型烴源巖、臺地內凹陷型烴源巖、深水緩坡與陸棚型烴源巖、深海盆地型烴源巖。
  13. It is a late cretaceous to tertiary basin located on the eastern part of the continental shelf of the east china sea ; it occupies an area of 59, 000 km2

    西湖凹陷是晚白堊第三紀盆地，位於中國東海大陸架的東部，面積590000km2 ，處于緯度124030 '與127000 '之間，經度28030 '與31000 '之間。
  14. In lucaogou period some regions even appeared terrestrial playa lake since the ratio of sr / ba even reached 42. 5

    中二疊世蘆草溝期馬朗凹陷局部地區還出現陸相干鹽湖特徵， sr / ba比值最高可達42 . 5 。
  15. 3. by means of sequence stratigraphy, the sequence frameworks of the permian in mahu depression have been established, which were divided into 5 sequences. and sedimentary system tracts have been studied

    3 、將層序地層學理論用於陸相環境，建立了瑪湖凹陷二疊系沉積層序格架，把二疊系劃分為5個層序，並通過測井資料對層序內部的體系域進行了分析。
  16. It is found that : ( 1 ) for linear slope, redistribution of incoming energy flux in modenumber space depends on both the modenumber of incident waves and the ratio of the slope of incident wave ray to slope of topography ; both the transmitted and reflected energy flux ( only for supercritical linear slope ) focus near one or two modenumbers ; for supercritical linear slope, the energy flux scattering to higher modenumbers becomes larger and the energy flux to lower modenumbers becomes smaller as the slope of incident wave ray comes near to slope of topography ; ( 2 ) for convex slope, energy flux is redistributed in wide - range modenumbers and also show peaks on lower - modenubers and higher - modenumbers ; ( 3 ) for concave slope, energy flux is also redistributed in wide - range modenumbers, but does not show peaks on higher - modenumbers as supercritical linear slope and convex slope do ; ( 4 ) the total energy flux scattering to higher modenumbers is approximately equal to the total energy flux to lower modenumbers for internal waves propagating over both convex slope and concave slope, which means the concave slope is the same efficient to convex slope in scattering energy flux to higher modenumbers ; ( 5 ) for convex slope, the wave ray reflected from near - critical topography can extend to deep ocean and shallow shelf, while for concave slope, the wave ray reflected from near - critical topography can only extend to limited distance, then meet the topography and be reflected again ; generally the shear of the internal waves reflected twice from concave slope is not enhanced while the enhanced shear does also appear before second reflection takes place, the enhanced shear can bring about intense mixing, so internal waves reflected from concave slope can also produce marked mixing near critical slope

    3 、內波在凹地形上傳播時，能通量在模態上的分佈范圍也比較寬，但與凸地形和超臨界線性斜坡地形相比，能通量在高模態上的分佈沒有明顯的峰值。 4 、從總的能通量來講，內波在凸地形和凹地形上傳播時，向高模態散射的能通量與向低模態散射的能通若十地形下內波傳播及內潮生成問題的理論解量近似相等，這意味著二者在向高模態散射能通量方面具有同等效率。 5 、凸地形上臨界點附近的反射，反射波的波射線能夠延伸到深海和陸架，凹地形上臨界點附近的反射，反射波的波射線很快遇到地形發生二次反射，一般來講二次反射后回到深海的波動其速度剪切並不很強，但是在進行二次反射之前的區域，速度剪切仍然很強，因而內波在凹地形上的反射依然能夠在地形附近區域，產生強的速度剪切區，誘發混合。
  17. In addition, by means of seismic profiles, the platform margin and the platform inner sag margin can be finally identified, integrated with distribution of organic reefs

    分析中上奧陶統烴源巖沉積環境，重要的是尋找碳酸鹽巖臺地邊緣、臺地內凹陷邊緣，從而能夠確定臺緣斜坡、臺地內凹陷、陸棚等烴源巖沉積環境。
  18. Formation conditions and distribution laws of oil reservoirs in luxi depression of eastern inner mongolia

    內蒙古東部陸西凹陷油氣成藏條件與分佈規律
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