geologic formation 中文意思是什麼
geologic formation
解釋
地質構成-
The geologic, element and experimental study suggest the mechanism of small body, giant deposit in jinchuan is succeeding segregation whole magma chamber intruding from deep to emplace. the study is proof, supplementary and progress of the deep segregation, penetrating ore formation theory, which was advanced by mr tang zhongli, the academician of china. 5
特別是通過鉑族元素、稀土元素研究、實驗地球化學研究及其與實際資料的對比，提出了金川礦床成巖成礦是從深部到侵位持續熔離的新模式，論證、補充和發展了湯中立院士提出的深部熔離成礦說。 -
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。 -
The first geologic reason for degeneration of the eco - environment in the headwater area of the yellow river is that the increase of the recent geologic function caused desertification and grasslands resource decreased and underside changed, destroied the balance of water - air - heat in the area ; the second is that the water environment changes by the degradation and atrophy of frozen earth cause multilayer and synthesis cause of formation degeneration of the eco - environment ; the third is that the man and rats function accelerated degeneration of the eco - environment in the headwater area of the yellow river
摘要黃河源區生態環境惡化的地質原因之一是現代地質作用增強，形成以荒漠化為主的草地資源退化與下墊面改變，地區水氣熱平衡破壞；二是因凍土退化、萎縮，引起水環境變異，導致多層面與綜合成因的生態環境惡化；三是人為及鼠類活動對源區生態環境惡化起著推波助瀾的作用。 -
The lake shore sandy dike in the shrinking process of " hetao ancient lake " in the geologic period, which is suffered from the wind force function " rises right on the sandy land ", is the substantial basis of the formation of maowusu sandy land
摘要地質歷史時期「河套古湖」退縮殘留的湖濱沙堤受風力作用「就地起沙」 ，是毛烏素沙地形成的物質基礎。 -
According to the research on volcanic rock reservoirs, the formation reasons of volcanic rock reservoirs, process of cognition, and the general geologic characteristics and the general development characteristics of volcanic rock reservoir are summarized
在調研了國內外火山巖油氣藏的基礎上，對火山巖形成油氣儲集層的原因進行了分析，對火山巖油氣藏的認識過程、一般地質特徵以及一般開采特徵進行了總結。 -
In the west qinling, qilian and longshoushan metallogenic zones, some larger - ultra larger mineral deposits were formed throughout a model of " bearing " in long course of geological evolution. studying their geologic setting of " formation " and condition of late " development " would help us to objectively realize rules for the metallization and enrichment and define reasonable thinking for research and plan for exploration
甘肅西秦嶺、祁連、龍首山等成礦帶的大型-超大型金屬礦床，是在地質構造發展演化過程中「生長」而成的；研究分析其「生」成背景與後期成「長」的條件，有利於客觀認識成礦與富集規律、合理確定研究思路與勘查方案等。 -
Based on the analysis of sedimentary facies in individual wells and the correlation of three cross sections of sedimentary facies, it is elaborated that sedimentary facies of jianglingjiang formation are vertically and laterally developed within qianwei area. by the method of single - factor analysis, it is pointed out facies distribution of four key formations after thorough study of four geologic factors that could embody sedimentary environment and facies, that is the thickness of formation, grainstone and dolostone, and lithofacies. with the above results, combining with reservoir and structural features, of which the emphasis is the reservoir characteristics of different rock and microfacies types, it is pointed out favorable reservoir zones, by the method of multi - factors superposition
採用單因素分析法，選取並研究地層厚度、顆粒巖厚度、白雲巖厚度和區域巖相等四種能反映沉積環境和沉積相的地質因素，指出了四個重點層段的沉積相平面分佈特徵；根據沉積相的研究成果，結合儲層特徵和構造發育特徵，著重討論了不同巖石類型和微相類型的儲集特徵，採用多因素疊合法對犍為地區嘉陵江組有利儲集相帶進行了預測，指出了有利儲集相帶的分佈。 -
The comparison study of the three belts indicates although they are distinct from each other all the three belts show many common features in the aspect of the metallogeny of large - rich vein uranium deposits, i. e : the important metallogenic areas are located above the old crystalline basement ; the paleo - rifting ( taphrogeny ) controls the development of the volcanic belt and at the same time it is favourable metallogenic tectonic environment ; the occurrence of uranium deposit does not depend on the lithology of volcanic rocks ; uranium metallogeny is obviously constrained by deep geologic processes and the connected fault - structural net is the necessary condition for the formation of large - rich uranium deposits
對比研究表明，雖然它們各具特色，就脈型富大鈾礦床成礦作用而言，它們又具有較多的共性：重要成礦區的火山噴發皆奠基在古老的結晶基底上；古裂谷（或裂陷）既控制了火山巖帶的發育，又是有利的成礦構造背景；鈾礦賦存對火山巖的巖性沒有明顯的選擇性；鈾成礦的深部控製作用明顯；聯通的構造網路系統是形成富大鈾礦的必要條件。 -
Abstract : the authors discuss roundly source of loose earth fo r impact - deposit debris flow to develop taking pingchuan debris flow, one of the quite typical impact - deposit debris flows in southwest sichuan province ， as an example in this paper. on the basis of detailed investigations in - situ, geotechn ial testing in lab and theory analysis, all results indicate obviously that moder ate and bulky loose earth in giant debris flow situating in southwest sichuan mo untainous area are main institute, whose tribulation are consistent with landform s. loose earth locating in mid - forepart catchment are quite unstable, so often be comes main source of loose earth of debris flow. formation of loose earth is cont rolled principally by geologic and geotechnical environment while human actions is the secondary factor for loose earth to form. in many times, human actions prov ide loose earth through loose earth stability
文摘:本文以極具典型的平川泥石流為例比較全面的分析了沖淤變動型泥石流的物源問題.根據現場調研及室內巖土分析進行的研究成果顯示，川西南高山深谷地區的大型泥石流溝中的鬆散土體以中、粗粒段為主，其分佈與地形密切相關；位於泥石流溝中、前部位的鬆散土體的穩定性最差，是補給泥石流的重要物源；鬆散土體的發育主要受控于地質及巖土環境，人類活動只能影響鬆散土體的穩定性 -
However, the geologic structure of the carstic formation is complicated and the design, construction, quality testing method of the high - pressure grouting is developing rapidly. we have engaged lots of experiments and studies in xiangshuiriver reservoir on this subject. one of the purposes subject is to guide the design, construction of the curtain grouting in the xiangshuiriver reservoir and optimize the grouting design, the other is to be a reference example for other similar engineering
但由於巖溶地質條件的復雜性，且高壓灌漿作為一項技術和工藝，在設計、施工、質量檢驗及效果評價等方面，仍然處在不斷發展的過程中，正是基於以上兩個方面的考慮，本課題結合響水河水庫高壓帷幕灌漿工程進行了大規模的試驗研究，一方面指導帷幕灌漿的設計與施工，達到優化設計方案的目的；另一方面對試驗資料進行分析研究，以期對同類工程有所助益。 -
The formation of large ore - concentated are results from the anomalous concentration of multi - mineral resources and large amount of ore materials during the process of geologic evolution history
大型礦集區的形成，是在地質歷史演化進程中，多礦種大礦量超常聚集的結果。 -
Based on the principles of palaeobiology, stratigraphic geology, sedimentology, diagenesis and reservoir geology, taken field profile and drilling cores as research object, and combined with achievement of predecessors, the sedimentary facies, diagenesis essential characteristics of reservoir and controlling factors for reservoir of feixianguang formation in northwest sichuan have been comprehensively studied. both classic and mordern methods have been used in this research. the main confents includes : stratigraphic classification and correlation of feixianguan formation in lower triassic, the rock fexture characteristics, type and forming conditions of rock ; determining dirtributary law of the sedimentary facies in vertical and horizontal direction and distribution in plane and the essetial contronling factors through correlation of sedimentary facies transverse profile and regionnal geologic characteristics ; establishing plane stereoscopic modle of sedimentary of oolitics beach by studying diagenesis
主要內容包括：對川西北地區下三疊統飛仙關組地層進行了劃分與對比，研究了飛仙關組地層的巖石結構組分特徵、類型和形成條件；通過沉積相橫向剖面的對比，並結合區域地質特徵，深入研究了沉積相在縱、橫向上的變化規律，確定了沉積相在平面上的分佈及主要控制因素，分析了沉積相的縱向演化過程和建立了沉積相的平面立體模式；詳細研究了該套地層所經歷的成巖作用類型、特徵及對儲集空間的影響，建立了鮞粒灘相儲層的形成與演化模式；最後，從沉積相、成巖作用的角度，分析了區內飛仙關組地層的生油潛力、儲層的分佈規律和發育區塊。 -
During interpolation, the original frequency of seismic signal is kept very well without negative effect to the subsequent processing. 5. cubic curves are used to geologic structure model input, and the formation boundary becomes smooth, which is good to the forward modeling. this method could hold true to various background
成功地將樣條曲線應用於地質模型輸入環節，保證了地質模型界面的光滑連續，並能夠廣泛適應于各種質量的模型底圖，為正演模擬取得良好的效果奠定了基礎。 -
This research apply the method of high accuracy sequences stratigraphy, and establish high accuracy geologic stratum trellis of shahejie formation s34 of shen 84 - an 12, identified 3 indicate layers. study on sedimentary microfacies is base of reservoir heterogeneity research
本次研究應用高精度層序地層方法，建立了沈84 ?安12塊沙河街組s _ 3 ~ 4段的高精度地層格架，識別了2個標志層。 -
Through the above process, the users will realize the geologic formation clearly. finally, the demonstration of this system has been build up by using parts of data. the results suggest it has high reliability and releases the uncertainty by using single geophysical techniques
最後利用部分勘探數據對軟體進行了測試和驗證，結果證明應用該系統進行物探成果的綜合解釋可信度高、減少了單一物探方法地質解釋的不確定性和多解性的弊端。 -
In different geologic development stage, different geodynamics background and tectonic stress field characteristic led to different baisin types, sedimentary assemblage. basin - mountain coupling forms and produced complex structure deforming. consequently, superimposed basin are characterized by multi - stage basin - formation, multi - stage hydrocarbon generation, multi - stage hydrocarbon accumulation. complex accumulation mode and oil / gas distribution law. tectonic process is key point and decisive in many hydrocarbon accumulation factors of superimposed basin
在不同的地質發展階段，由於不同的地球動力學背景和構造應力場特徵，導致了不同的盆地類型、沉積組合、邊界條件和盆山耦合形式，產生了復雜的構造變形，從而使疊合盆地具有多期成盆、多期成烴、多期成藏以及復雜的油氣成藏模式和油氣分佈規律。 -
Based on the analysis of geological condition and hydro - geologic condition as well as the initial survey 、 design and construction of a highway slope the reason of developing formation of this high - way landslide is explored to reveal some parts of landslide mechanism and the construction impact on slope stability, finally some reasonable suggestions are presented for highway survey design and construction
摘要通過對某高速公路滑坡的復雜的地質條件，水文地質狀況及初次勘察、設計、施工的分析，說明了該公路滑坡事故形成的原因，揭示了公路滑坡形成的部分機理和工程建設對邊坡穩定性的影響，對公路工程建設中的勘察、設計及施工提出了合理的建議。 -
( 5 ) discovered a abnormal law that the sonic velocity was enlarged with increasing of die core porosity in the sandstone reservoir of the haojiagou formation in triassic, and gave a geologic interpretation about the phenomenon. it was helpful to convert the sonic velocity into die porosity correctly in reservoir. ( 6 ) gave a primary reason for producing a little oil and gas in the well ha - 2 and ha - 3 of the sidaogou structure
通過取心段地層巖性與聲波測井速度分析，首次發現郝家溝組儲層段巖芯孔隙度與聲波時差（聲波速度）存在反常變化規律，並對這種現象進行了較合理的地質解釋；提出了儲層預測中應注意的問題，首次提出在本區按常規方法利用聲波時差換算孔隙度存在陷阱。 -
Abstract : the yellow river delta is an ideal nature location to research geologic environment evolution, since the new land formation rate is the fastest and continue rapidly expand in china or even in the world
摘要:黃河三角洲是中國面積最大、形成時間最晚、發展速度最快且仍在繼續發展的三角洲平原，是研究海岸帶地質環境變化的理想場所之一。 -
Located in or facing the path of an oncoming glacier. used of a geologic formation
冰川運動路線的位於或面對冰川運動路線的。用於地質構造
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