anomaly source 中文意思是什麼
anomaly source
解釋
異常源-
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。 -
A glide correlation analytical method for gravity and magnetic anomaly is advanced in the paper, with some application examples given, such as estimation of the nature of the anomalous source, division of oil prospects, and delimitation of boundaries of tectonic units
摘要給出了一種重磁異常滑動相關分析方法，並例舉了在重磁異常源性質判斷、油氣遠景區劃分、構造單元邊界劃分等方面的運用實例。 -
Using the daily and monthly ncep / ncar reanalysis data from 1951 to 2000 and monthly precipitation of 160 stations in china in summer from 1951 to 2000, the climatic distribution of heat source are computed. the responses of the asian monsoon circulation to the annual anomaly of the heat source over the bay of bengal in summer and the annual relationship between the heat source and the precipitation of china in summer are analyzed
摘要利用1951 - 2000年ncep / ncar再分析逐日及月平均資料和我國160個測站1951 - 2000年月降水量資料，計算了夏季大氣熱源氣候分佈，分析了夏季孟加拉灣地區熱源年際異常及亞洲季風環流系統的響應，以及夏季孟加拉灣地區熱源與中國夏季降水的年際關系。 -
Analyzing on sequence characteristics, earthquake source, medium rupture characteristics, source conditions, historical seismicity, regional earthquakes and anomaly change of precursor data, etc., we know well regional background of seismic activity before the m ( subscript s ) 6. 1 the earthquake and judge earthquake situation trend after the m ( subscript s ) 6. 1 the earthquake
摘要通過分析昭蘇6 . 1級地震序列特徵、震源與介質破裂特性、震源環境與歷史地震活動類比及區域地震和前兆資料的異常變化等，對該震前的區域地震活動背景、震后的震情趨勢等有了較為細致的了解和判定。 -
The source of the anomaly may lie in this region rather than in the highpressure film.
反常現象的起源可能在這個區域，而不是在高壓油膜區。 -
Based the basic principle of the accumulation of induced electric charges across the resistivity discontinuities and the induction current channeling inside the conductive bodies inspirited by the mt field, we set up the relation between the measured field on the earth surface and the distribution of the induced source underground by means of the defining the electric charge occurrence probability function and the electric dipole occurrence probability function and the spacial distributing of the " correlation probability ". the " image " of the field sources underground, or the distributing graphy of the induced electric charges and the induced current in the mesuring area can be drawed, from which we can get the outline of the geological anomaly on the meaning of the probability
大地電磁場概率成像方法是一種新的地球物理成像反演方法，它是根據在大電磁波場的激勵下，地下介質電阻率間斷處產生感應電荷積累和導體內部產生感應電流，從而產生感應電磁場的原理，相應地定義了感應電荷發生概率函數和感應電偶極子發生概率函數，通過「相關概率」發生的大小的空間分佈，建立了地表觀測場與地下場源空間分佈的內在聯系。地下場源分佈概率的「像」 ，即測區的感應電荷和感應電流的概率的分布圖像，就是測區內地質體在概率意義下地質異常體的分佈輪廓。 -
It is often impossible to differentiate between structure and density contrast in determining the source of a gravity anomaly.
在確定重力異常源時，不可能在構造與密度差之間作出抉擇。 -
There must be a substantial anomaly in the system to make such activities worthwhile ; the most likely source is the way ratings are treated
擔保債券局深諳此道，重新包裝了現行的債券，並掌控了大部分收入. 。 -
It was showed that the fractal characteristics of magnetic anomaly reflects the variations of physical factors of subsurface magnetic source, and is affected by the burying depth and extending depth of the source
分析認為磁異常具有分形結構，分維值與淺源磁化率分佈有關，並受其埋深、延深等幾何因素的影響。 -
The pb isotopic ratios show the characteristic of dupal anomaly and influence of ocean sediment to the source
Pb同位素研究也顯示了dupal異常型的特徵以及大洋沉積物對源區的影響。 -
Pb isotopic features imply that its source is similar to that of the indian ocean morb, and a dupal anomaly
Ph同位素特徵表明其源區類似於印度洋morb的源區，具有dupal異常型的特徵。 -
Vector characteristics of magnetic anomaly measured in drill holes can be used to determine the strike of magnetic source that results in the magnetic anomaly
摘要利用井中磁異常矢量分佈特徵能確定引起該異常磁源的走向。 -
According to the means of detection intrusion, ids can be divided into signature - based detection and anomaly detection, signature based ids also is called misuse ids. according its deployment and data source, ids also is divided into network based and host based detection
它從檢測入侵所使用的分析技術來說可分為基於異常行為的入侵檢測和基於特徵的入侵檢測（也叫誤用檢測） ；而從數據來源及配置上又可分為基於主機的入侵檢測系統和基於網路的入侵檢測系統。 -
It is source of blazing new trails, basis of seeking orders, much important to the multi - objective mineral prediction and assessment based on systematic studies of the inhomogeneity, diversity, variety, intergrowth law, multiple properties and uses of earth mineral resources, the multi - objective mineral prediction and assessment goes deeply into practice from seeking anomaly or / and difference to order or / and law of ore - forming
求異是創新之源、求序之本，更是多目標礦產預測評價之關鍵。充分認識地球礦物質組成的不均一性、多樣性、多變性、共生性和多用性等特徵與規律，在求異的基礎上求序，在求序的指導下進行科學預測與評價。 -
By the detecting technique utilized, intrusion detection systems can be classified as misuse detection systems and anomaly detection systems ; according to the source of data, intrusion detection systems can be grouped into host - based and network - based systems
從所採用的技術看，入侵檢測系統大致可分為誤用檢測和異常檢測兩大類；從檢測數據的來源看，又可分為基於主機的和基於網路的兩種。
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