shallow source 中文意思是什麼

shallow source 解釋
淺源
  • shallow : adj 1 (shallower; shallowest) (水、器物等)淺的。2 薄的。3 膚淺的;表面的;皮毛的。4 (呼吸)...
  • source : n 1 源頭,水源,源泉。2 根源,本源;來源。3 原因;出處;原始資料。4 提供消息的人。5 血統。vt 〈美...
  1. The causes are discussed from aspects of oil - gas source beds, trapping and storing space, oil - gas migration channel and thick proofing layers, oil - gas maturity stage and allocation of effective trapping stage, suggesting the searching of primary oil - gas pool of the cambrian and lower ordovician at the relatively shallow layers and surrounding places with faults developed

    從油氣源層、圈閉與儲集空間、油氣運移通道與巨厚隔層、油氣成熟期與圈閉有效期配置等四個方面探討了未獲油氣之原因,提示在滿加爾坳陷腹地,相對較淺部位及周邊斷裂發育部位尋找寒武系和下奧陶統的原生油氣藏。
  2. Tncyclic diterpanes c20, c21 and c23 distribution also has relationship with oil gravity, oil and gas production, as well as oil pool formation timing and oil source. rising - patterned oil originates from fengcheng formation, while peak - patterned oil from xiawuerhe formation. four types of migration and accumulation models are put forward : ( l ) fault controlled migration and accumulation along ridge far from source region ; ( 2 ) fault and unconformity controlled migration and accumulation around source region ; ( 3 ) fault controlled migration and accumulation in the slopes within source region ; ( 4 ) biogenetic and low temperature catalyzed gas migration and accumulation in middle and shallow formation

    受擠壓背景控制,研究區內海西期形成的斷裂,全部為逆斷裂,活動期長,可以延續到印支期和燕山期,斷開層位可以從石炭繫上延至誅羅系,它們對區域構造、沉積、油氣運聚有顯著的控製作用;而燕山期形成的斷裂多為小型正斷裂,部分為株羅系和白要系內部斷裂,部分從徐羅系斷至白聖系。
  3. Gas hydrate ? a source of shallow water flow

    天然氣水合物:淺水水流之源?
  4. Based on the hydrodynamic energy transport model, the influence of variation of negative junction depth caused by concave depth on the characteristics of deep - sub - micron pmosfet has been studied. the results are explained by the interior physical mechanism and compared with that caused by the source / drain depth. research results indicate that with the increase of negative junction depth ( due to the increase of groove depth ), the threshold voltage increases, the sub - threshold characteristics and the drain current driving capability degrade, and the hot carrier immunity becomes better in deep - sub - micron pmosfet. the short - channel - effect suppression and hot - carrier - effect immunity are better, while the degradation of drain current driving ability is smaller than those with the increase of depth of negative junction caused by source / drain junction shallow. so the variation of concave depth is of great advantage to improve the characteristics of grooved - gate mosfet

    基於能量輸運模型對由凹槽深度改變引起的負結深的變化對深亞微米槽柵pmosfet性能的影響進行了分析,對所得結果從器件內部物理機制上進行了討論,最後與由漏源結深變化導致的負結深的改變對器件特性的影響進行了對比.研究結果表明隨著負結深(凹槽深度)的增大,槽柵器件的閾值電壓升高,亞閾斜率退化,漏極驅動能力減弱,器件短溝道效應的抑制更為有效,抗熱載流子性能的提高較大,且器件的漏極驅動能力的退化要比改變結深小.因此,改變槽深加大負結深更有利於器件性能的提高
  5. Firstly, based on the basin prototype, the triassic and jurassic mudstone and coal, the main source rocks of the basin, did not develop better in baicheng sag than in the northern thrust belt including keyi structural belt ; secondly, because of the thrusting happened in late cenozoic, the triassic and jurassic source rocks reach to a high to over high maturity and thus generate gas or condensate oil mainly. thirdly, the thrust faults compelled the natural gas to migrate from the north to the south or from the deep to the shallow. as a result, the keyi structural belt and the eastern qiulitage structural belt enriched in natural gas because they were not only located on the migration routines of the natural gas, but also developed simultaneously when the gas migration happened

    從盆地構造史研究的角度認為庫車盆地的天然氣主要來源於北部山前沖斷帶: 1受原型盆地構造格局的制約,三疊系侏羅系烴源巖發育的最有利位置不是在拜城凹陷,而是在克依構造帶及其以北的北部山前沖斷帶2晚第三紀以來的逆沖推覆作用使得烴源巖提早進入高過成熟階段,並以產氣和凝析油為主3逆沖推覆作用所產生的北傾逆斷層控制天然氣自下而上自北而南運移,位於運移路線上的克依構造帶和秋里塔格構造帶的東段與烴源巖的排氣期匹配較好,從而使這些地區最富集天然氣。
  6. Three sets of source rocks had been formed juring the steady sinking of the basin. the first source rock, being clay and calcium clay stone in tiemulike formation of permian was formed in deep lake environment ; the second source rock, being clay stone in xiaoquangou group of middle to upper triassic was formed in the offshore and the shallow lake environment ; and the third source rock, being coal beds in badaowan formation of lower jurassic was formed in the lake - swamp environment. the first one is the most potential, since it has the biggest thickness, the highest organic matter abundance, high maturity and the highest hydrogen generating capacity

    在盆地穩定沉降時期,相應地形成三套烴源巖,即上二疊統鐵木里克組( p _ ( 2t ) )深湖、半深湖相泥巖、泥灰巖;中上三疊統小泉溝群( t _ ( 2 - 3xq ) )濱淺湖相泥巖及下侏羅統八道灣組( j _ ( 1b ) )湖沼相煤系地層。
  7. According to different water phenomena, we use two different method to produce waves source : the first method is by specifying the boundary conditions and initialization conditions, this method simulate the dam breaking, reflection and diffraction of water waves ; the second method is by specifying disturbance model, this method simulate water droplets, waterfall, waves of ship ; in the first part of this thesis, we discuss the prevalent methods of the simulation of water scenes, in the second part of this thesis, we describe the numerical methods of solving the shallow water equations using the finite difference method and the finite volume method respectively, in the third part of this thesis, we simulate some realistically liquid phenomena such as rain droplets, the waves of ship, dam breaking etc

    產生水波首先要有波源,設置不同的波源便可以得到不同的水流情形,我們用兩種方法來產生波源:一種是通過設置邊界條件和初始條件產生,這種方法用於模擬潰壩波的反射、折射等現象;另一種是通過擾動控制產生,這種方法用於模擬雨滴、瀑布、船波等自然現象。本論文的第一部分我們討論了目前水動畫模擬常用的幾種方法;在第二部分討論了我們所使用的兩類數值方法:有限差分方法和有限體積方法;在第三部分我們模擬了雨滴、船波、潰壩波等一些水流現象。
  8. Characterization of source rock of shallow tight sand gas in dongliang district in the fuxin basin

    阜新盆地東梁區淺層緻密砂巖氣氣源巖特徵
  9. When you are devising a long - term water source for your garden, plan for the type of water feature that birds adopt most quickly : a shallow, rough - bottomed pool of still water

    當你計劃在院子里給鳥類提供一個長期的飲用水源時,你應該將它設計成最易於為鳥類所適應的? ?它應該是淺的、具有粗糙硬底的靜水。
  10. Have evolved deep under the oceans at hydrothermal vents, where volcanic fluids rich in reduced chemicals served as an energy source, or in shallow geothermally heated waters on earth s surface, where these chemicals or sunlight could have provided an energy source for

    這類生物可能在深海中的熱液火山口處演化,那裡的熔液含有豐富還原化學物,提供了生長和復制所需的能量又或在地球表面受地溫加熱的淺水處演化,從陽光或水中的化學物中攫取能源。
  11. The distributions of source rocks, reserviors and faults / fissures, and conservation are the critical factors in poolforming and enrichment of gas in the foreland basin. 6. the thrust belts of longmen mountains are potential prospects in the basin with the concentrated structural traps, strucrural - fissuring traps, and faults connecting between the shallow and middle formations

    6 、龍門山山前沖斷帶具有較大的油氣潛力,構造圈閉、構造-裂縫型圈閉發育,中淺層構造同步發育或有斷裂溝通,具有中淺層均含氣的特徵。
  12. Shallow talk about the light source of intermediate vision standard

    在汽車照明系統中的應用
  13. Creates a shallow copy of a range of elements in the source list

    中的元素范圍的淺表副本。
  14. As results of mix of deep mantle - source materials and shallow metallogenic materials, and tectonic movement of south unit and north unit, dongxiang copper deposit become a multi - metal deposit especially enriching cu, together with fe, w, s, ag, au, bi, cs and te etc. 2. ore - forming of copper deposit has much to do with the geotectonic of deposit area

    深部的幔源物質與淺部的成礦物質混合,南北兩大構造單元各自的成礦特徵又在此集中體現,使東鄉銅礦成為一個以銅為主,伴生鐵、鎢、硫、銀、金、鉍、銫、碲等元素的多金屬礦床; 2
  15. The effect of an anisotropic field of internal waves on the localization of the interference pattern in a shallow sea is analyzed in the range of 100 ? 320 hz for different distances from the source ( up to 100 km )

    在淺海乾涉模型定位方面的應用,對應距離從來源(最大100公里)的不同的距離,各向異性場曲率內波的的應用范圍,在100 320赫茲范圍。
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