residual basin 中文意思是什麼
residual basin
解釋
殘留盆地-
The pges abundance patterns of residual mantle rock with a peleo - subduction background is characterized by pd, pt depletion and ir, ru relatively enrichment, while the basalt and basic dyke by the processing of partial melt in the same background take an opposite feature of pd, pt enrichment and ir, ru depletion. the existence of fluid in the subduction zone increases the degree of partial melt on the one hand, and on the other, activates the activity of pd, pt compare to ir, ru, and thus reduces the pd ir and pt ru in residual mantle rock. the pges patterns for basalt and basic dyke from two carboniferous volcano zones to south qoltag and north turpan - hami basin, xinjing uigur autonomous region, take a shape of gentle positive inclined curve with lower pt and pd differentiation and lower pges. all these features are obviously different from that of basic dyke and basalt from typical ophiolite and therefore the author believe that their fluid - rich paleo - subduction zone environment can be ruled out
古俯沖帶背景下的殘餘地幔巖的pges配分以pd ， pt明顯虧損和ir ， ru相對富集為特徵，而部分熔融產物的玄武巖和基性巖脈則呈現相反的ir ， ru明顯虧損和pd ， pt相對富集特徵。俯沖帶中流體的參與一方面增加了部分熔融程度，有利於pd ， pt從原始地幔進入熔融相另一方面，流體的作用使得pd ， pt相對于ir ， ru遷移活動性效率提高，造成地幔巖中 -
The peripheral basin is a residual coincident basin which experienced a strong reform, and is a reserves replacement area for daqing oilfield
摘要外圍盆地是經歷強烈改造的殘留型疊合盆地，大慶油田公司長遠戰略接替區。 -
During this evolution, seven second - order tectonic units were formed ; from north to south are the mingqianri cretaceous residual sea basin, the arsuo tectonic melange zone, the taricuo - wenbu yenshan magmatic arc belt, the cuoqin - bangduo late paleozoic composite back - arc basin, the jiangrang - geerdi faulted uplift, the gangdise - chazi himalayan magmatic arc belt, and the xigaze - anba fore - arc basin. these units comprise important parts of a poly - arc - basin system and exhibit evolutional features of mesozoic to cenozoic arc - basin systems. mosaic pattern of these tectonic units delineates the lithosphere coupling processes of the gangdise tectonic belt under mechanisms such as back - arc basin attenuation and arc - continent collision
自中新生代以來，岡底斯構造帶經歷了洋殼俯沖、弧陸碰撞、陸內俯沖-碰撞、走滑和塊段隆升的多階段構造演化歷程，形成了由北向南七個二級構造單元，即岷千日白堊紀殘余海盆、阿索構造混雜巖帶、它日錯?文部燕山期巖漿弧帶、措勤?幫多晚古生代復合弧后盆地、江讓?格爾耿斷隆、岡底斯?查孜喜馬拉雅期巖漿弧帶、日喀則?安巴弧前盆地。 -
According to the chemical experimental data of residual organic carbon content, kerogen carbon isotope, aliphaltic gas chromatography mass spectrometry of 67 outcrop specimens in the baise basin, the authors analyse the geochemical characteristics of the type and the maturation of organic matter in the lower triassic - devonian source rock
根據百色盆地周緣大量露頭樣品的殘余有機碳含量、乾酪根碳同位素、飽和烴色譜及色質等地球化學實驗數據，分析了下三疊統泥盆系海相烴源巖的有機質豐度、類型、熱演化程度。 -
Yanqi basin is a typical reformed residual basin where several oil and gas fields with commercial value and some product energy have been found in recent years
焉耆盆地是一典型的改造殘留盆地，在其中已發現多個有商業價值和一定規模產能的油氣田。 -
Based on the light hydrocarbon compositions and the distributions of n - alkanes and the oil physical features, the genetic mechanisms of the pristine oils, residual oils and retrograde oils in yaha area are discussed, which identified the existence of second gas - condensate reservoirs in the kuche basin
四種不同性質、不同成因的油氣藏共存於同一構造帶上，通過油藏地球化學的精細剖析，較好地理解了這一復雜的過程，顯示了油藏地球化學在油藏形成機理研究中的潛力。 -
The base of studying original appearance and its dynamic evolution is sedimentary body of residual basin
殘留盆地的沉積實體是研究盆地原始面貌和動態演化的基礎。 -
In a room containing a bath or shower, the provision of socket outlets should comply with iec 60364 - 7 - 701 ( to be installed at location 0. 6 m away from shower basin or bath tub ) and the socket outlets should be protected by a residual current protective device ( rcd ) with a residual operating current not exceeding 30ma
設有浴缸或花灑的浴室內，插座應符合國際標準iec60364 - 7 - 701的規定（包括安裝的位置距離浴盆或浴缸0 . 6米以外） ，並由餘差啟動電流不超過30毫安的電流式漏電斷路器加以保護。 -
By the comparison of the residual strata, sedimentary evolution and source rocks among kuche depression, kumishi basin, u ' erdusi basin and yanqi basin, die result shows that mesozoic sedimentary environment of these basins has tightly relationship which all belongs to tarim basin
通過將塔里木盆地北部庫車坳陷地層、沉積演化和烴源巖以及庫米什盆地、尤爾都斯盆地殘留中生代地層與焉耆盆地的對比研究認為，庫車、焉耆、尤爾都斯及庫米什盆地在中生代沉積環境彼此相關，均屬大型塔里木中生代盆地的有機組成部分。
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