top of formation 中文意思是什麼
top of formation
解釋
地層頂板-
Based on analysis of geologic foundation record about pingzhuang basin, a lot of sino - foreign geothermal geology record and investigation of field geology, measuring of ground temperature in person and geo - chemical analysis of ascension spring, gushing water of fault, the fact that the anomaly of geothermal gradient of pingzhuang basin, which is in region of low geothermal gradient, is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out. after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys, the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed. the sound condition of transmissibility fault and feeding water source, which are imperative in formation of the low - medium temperature geothermal system of convective type, is possessed in pingzhuang basin
通過對平莊盆地基礎地質資料、國內外大量地熱地質資料的分析和野外地質調查、礦井實測地溫以及上升泉、斷層涌水的地球化學分析等工作基礎上，指出地處低地溫梯度背景區的平莊盆地地溫梯度異常是由於盆地基底隆起和坳陷引起傳導型大地熱流再分配所致；運用州sys數值模擬了大地熱流向地表傳導背景下的盆地地溫場，從而揭示了盆地基底（義縣組）頂界面地溫分佈特徵；闡明了盆地具有形成中低溫對流型地熱系統所必需的導水斷裂、補給水源等的良好條件，中低溫對流型地熱系統是地熱勘查的主要對象；圈定了平莊盆地北部朝陽溝?駱駝營子地熱勘查遠景區。 -
However, the authors discovered recently that the top and bottom surfaces of the loushanguan formation are palaeokarst unconformity interfaces, and there are a lot of interbeds of granular ( oolite, pisolite and oncolite ) dolomite and algae - mat dolomite, especially sedimentary structures such as the bird ? s eye, stromatolite, cross bedding and tepee structures
但筆者新近研究發現，其頂、底均為古巖溶不整合面，並有大量顆粒（鮞、豆、核形石）白雲巖和藻紋層白雲巖夾層，還有許多鳥眼構造、疊層石構造、交錯層理、帳蓬構造存在。 -
When soil antecedent condition is dry and the initial rainfall intensity is high, peak surface runoff also considerably lag behind that of rainfall, because of the formation of temporary relative impermeable top layer ; b ) surface runoff is controlled primarily by infiltration - excess runoff mechanism under unsaturated condition ; the major fraction of surface runoff are dominated by saturated infiltration - excess runoff response, only a small fraction by return flow mechanism when soil is saturated ; c ) subsurface flow is dominated by saturated runoff mechanism, and the duration of subsurface post the rainfall end is dependent upon rather the soil properties than the rainfall characteristics ; d ) subsurface flow intensity in cultivated soil layer ( 0 ~ 20cm ) is high up to 35mm / h when rainfall intensity is up to 120mm / h, indicating the existing of macropores and pipe flow in cultivated layer
2 ）耕作制下紫色土的產流主要機制是： 1 ）當雨前土壤含水量未達到飽和狀態時，表面產流起始時間有明顯滯后現象，這與紫色土的快吸水性和較多非毛管孔隙密切相關；當雨前土壤較乾燥，降雨初期雨強較大時，易形成臨時相對不透水表層，表面產流峰也有明顯滯后現象。 2 ）表面徑流的產流方式主要是超滲產流，當土壤達到飽和狀態后，有四川大學博士學位論文小部分回歸流發生，但主要是飽和超滲產流發生，因為紫色土的相對不透水層和其它透水障礙層不明顯。 3 ）壤中流主要是飽和產流，與降雨過程有明顯的滯后，而且雨停后的壤中流產流歷時與降雨特徵無關。 -
The scientific man is interested in finding out the chemical composition of the inside and crust of the earth upon which he lives, the thickness of the atmosphere surrounding it, the quantity and nature of cosmic rays dashing about on the top layers of the atmosphere, the formation of its hills and rocks, and the law governing life in general
在科學方面，人類所想要發現的，就是他所居住的地球的內部和外層的化學成分，地球四周的空氣的密度，那些在空氣上層活動著的宇宙線的數量和性質，山與石的構成，以及統御著一般生命的定律。 -
These enzymes are significant as a digestive aid to larval fish, improving survival and enhancing growth. sick and stressed fish are also beneficiaries of these enzymes. genchem polytase is our top of the line product, genchem polytase is a compound of several enzymes, rhizoma coptidis and cortex phellodendri extracts which can speedily and safely dissolve left - over feed, thus solving the problem of sediment formation and the stress caused by nitrous or ammonia
維生消化素也是消化整腸酵素，經由多種酵素及黃蓮，黃柏抽出物的綜合體，因為是多種酵素的組合所以能迅速分解殘餌，完全解決污泥的產生，免除亞硝酸及阿摩尼亞所造成的緊迫甚至泛池，更因為神奇的酵素作用能預防及免除使擾亂幼蝦正常代謝的生化與營養變化物質，而獲得幫助蝦苗消化酵素分化的正常機能，提高飼料效率，增加存活率防止疾病。 -
The rule represents the tectonic evolution feature ' s controling to the depositional infilling styles and facies " distribution. in dawan area, the top and the middle strata of the shahejie formation also developed a set of fan - delta sediment similar to the bottom of the shahejie formation, but the scale is significantly smaller
本區主要發育了兩套烴源巖，即沙三中段的暗色泥巖和沙三上段的煤系地層，它們在工區的兩個主要生油窪陷?於家房子窪陷和黃沙坨窪陷都有分佈，且厚度巨大。 -
The unconformability between the loess landform of shaanbei loess plateau and its bedrock shape was pointed out first after the full demonstration. the top of loess formation of the south part in shaanbei is flat which likes " platform ", the shape of the bedrock is rolling that likes ridge, and the bedrock bended to fold. the top of loess formation of the mid - part in shaanbei is rolling, but the shape of the bedrock below begins to get flat, the top of loess formation of the north part in shaanbei, loess mao district, is much more rolling among them, however, its shape of the bedrock below is the flattest relatively likes the platform shape of loess formation in south
具體地講，陜北高原南部的洛） 11黃土源，黃上層頂部相對平坦，地貌類型以黃土源為主格調，而其下伏基巖地層詔皺相對發育，古地勢起伏相對較大：陜北高原中部的延安一安塞黃土梁狀（為主）丘陵溝壑區，黃土層頂部起伏相對增大，地貌類型以黃土梁為主格調，而其下伏基巖地層槽皺程度趨弱，地層較平緩，古地勢起伏相對降低；陜北高原北部的綏德一子洲黃土赤狀（為主）丘陵溝壑區，黃土層頂部起伏度相對最大，地貌類型以黃上赤為主格調，而其下伏基底地層以平緩為特徵，古地勢起伏強度亦相對較低。 -
Most of this area was shallow - lake, semi - deep lake and deep lake sedimentary environment, except that the area around the well ou44 was a set of steep - slope fan - delta and the dawan area was a set of small - scale fan - delta. there were fan - delta, turbidite - fan, shallow - lake, shore - marsh, semideep - lake and volcano - debris facies. in the area of the well ou39 and ou44, fan - deltas developed both in the middle and the top strata of the third member of the shahejie formation
研究表明，粗面巖sio _ 2含量較高，流動性小，容易形成巨厚的巖鐘或巖錐，對成藏有利，同時其位於構造高部位，由於其大部在水面之上，冷卻時間長，易於從容結晶，同時還有大量裂縫作為儲集和滲濾的空間，使其成為良好的儲層。 -
The relationship between drawing top limitation and characteristics of scallop formation and thickness irregularity along article perimeter is found
確定了極限拉伸程度與齒槽形成特性和零件周邊壁厚差特性間的關系。 -
Lam was waiting on top of a steep rock formation to capture a sunset in north korea
有次在北韓，他爬上陡峭巖層的頂端等待，好捕捉曰落畫面。 -
There were fan - delta, turbidite - fan, shallow - lake, shore - marsh, semideep - lake and volcano - debris facies. in the area of the well ou39 and ou44, fan - deltas developed both in the middle and the top strata of the third member of the shahejie formation. the former lies in the north area of the well ou39, belonging to the steep - slope style which was controled by inertia factor
在歐39 、歐44井區，沙三中和沙三上均發育扇三角洲沉積，前者具以慣性因素控制的陡坡型為特點，分佈范圍相對較小，位於歐39井以北的地區；而後者以摩擦因素控制的緩坡型為特色，分佈范圍廣；而沙三下在該區則發育了一套濁積扇體，這一規律正好體現了構造演化特點對沉積充填型式及相展布的控製作用。 -
Both financials and non - financials, as the results of decomposition from top to tee, come from corporate strategies, and then a two - way cycle of formation and improvement between strategies and goals come into being
這些財務與非財務的考核指標都來源於企業的戰略，是對它們自上而下進行分解的結果。這樣，在戰略與目標之間就形成了一個雙向的形成與改進循環。 -
Both financials and non - financials, as the results of decomposition from top to toe, come from corporate strategies, and then a two - way cycle of formation and improvement between strategies and goals come into being
這些財務與非財務的考核指標都來源於企業的戰略，是對他們自上而下進行分解的結果，這樣，在戰略與目標之間就形成了一個雙向的形成與改進循環。 -
The formation of coral - like nano - structures was revealed on the top surface of zno films, while the existence of disk - like micro - structures was found on the inner surface that attached on mica
研究發現氧化鋅膜上表面具有納米尺度的叢生珊瑚狀結構，而與雲母接觸的下表面具有圓餅狀結構。
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