ore belt 中文意思是什麼

ore belt 解釋
礦帶
  • ore : n. 礦；礦砂，礦石；〈詩〉金屬（尤指貴金屬）。 be in ore 含有礦物。n. （pl. ore）1. 歐爾〈瑞典貨幣單位，等於1/100克朗〉。2. 歐爾硬幣。
  • belt : n 1 帶，皮帶；綬帶；線條；帶狀物。2 【機械工程】傳動帶；【天文學】雲狀帶；【軍事】子彈帶；腰皮帶...
  1. At the same time, the thesis has also made a discuss about the genesis of the ore belt, and brings forward a new cognition that partial aurum comes from the mantle

    同時，論文還在膠東地區礦床成因問題上做了探討，並提出了本區金礦物質部分來源於幔源的新認識。
  2. This article analyzes the mineralization mechanism of the uranium ore, constructs a series of spectra indexes including the ferric oxide index, the ferrous oxide index, the oxidation index, clay mineral index, brightness index, the green index and the humidity index, and draws the distribution and scope of the oxidation belt, deoxidation belt, the supplies and partial drainage of ground water in the research area, thus selects the advantageous area of uranium mineralization

    通過分析鈾礦的成礦機理，構建了氧化鐵指數、氧化亞鐵指數、氧化指數、粘土礦物指數、亮度指數、綠度指數和濕度指數等一系列光譜指數，提取了研究區氧化帶、還原帶、地下水補給與局部排泄的分佈和范圍，從而圈定了鈾礦成礦的有利區。
  3. Xiongcun copper - gold ore deposit is located in gangdese metallogenetic belt with a large scale. the ore body mainly exists in the second lithoid unit ' s tuffs and the third lithoid unit ' s dacite tufa of the cretaceous volcanic stratum, which are not only mother rock but also mineralized body

    雄村銅金礦床處于岡底斯成礦帶，礦床規模巨大，礦體主要賦存於白堊系火山巖地層第二巖性單元的黃鐵絹英巖化硅化凝灰巖和第三巖性單元英安質疑灰巖中，上述巖石既是賦礦圍巖又是礦化體。
  4. This paper describes the regional tectonics, ore deposit geological structure and geochemistry of the ultragiant streltzov uranium deposit in russia and its tectono - magmatic activization ore control, and points out its important practical significance for the metallogenic researches and prospection and exploration for the same type of uranium deposits in the jiangxi - hangzhou volcanic belt of china

    摘要文章介紹了俄羅斯超大型斯特列佐夫斯克鈾礦床區域構造、礦床地質構造和礦床地球化學特徵及其構造巖漿活化控礦規律，指出它對我國贛杭火山帶同類型的鈾礦床的成礦規律研究和找礦勘探有重要的實際意義。
  5. This paper discusses the evolution, metallogenic law, and ore - prospecting direction about the jiangda tectonic belt, by studying tectonic evolution and tectonics - metallogeny coupling relationship, guiding by theories of terrane - plate tectonics and tectonics - metallogeny, basing on the thought that different tectonic regime has different geologic - metallogenesis, and the conversion of multiple tectonic regimes conduces certainly to the generalized homothetic composite action of multiple metallogenic subsystems, and forming the multiple - composite metallogenic system

    本文以地體?板塊構造理論和構造成礦學理論為指導，通過深入研究江達構造帶的構造演化及構造?成礦耦合關系，本著不同構造體制具有不同地質?成礦作用，多種構造體制演繹導致多元（個）成礦體系的廣義同位復合構成多元復合成礦系統的思想，對江達構造帶的構造演化、成礦規律和找礦方向進行了系統的研究。
  6. And the generalized homothetic composite action of metallogenic subsystems mentioned above formed the multiple - composite metallogenic system of the jiangda tectonic belt. the typical ore deposits of jiangda tectonic belt, such as dingqinnong, jiaduoling, renda etc, are contact metasomatic type deposits formed intracontinental rifting stage, and the tectonic - magmatic - hydrotherm of intracontinental orogenic stage superposed and rebuilt some preexistent ore body. their space distribution is controlled by composite intrusive rock belt of ne direction

    對丁欽弄、加多嶺、仁達等典型礦床的研究表明，它們均為形成於陸內裂谷作用階段的接觸交代型礦床，陸內造山期的構造?巖漿?熱液作用疊加改造了先成礦體，礦床空間分佈受北東向復合侵入巖帶控制。
  7. In himalayan, the first era ( 45ma ) the basin is titled ; the second era ( 23ma ) it is differential uplift and denude ; the third era it is brittle defonnation. in eastern ore belt, ore - controlling is mainly strike - slip fault and fold ; but in western ore belt, it is block

    喜馬拉雅運動第一期45ma盆地掀斜；第二期23ma以差異隆升剝蝕為主；第三期4ma為脆性變形期，東礦帶近盆邊以走向斷裂及褶皺控礦為主，西礦帶為斷塊控礦。
  8. The discourse discusses structure pattern, rupture - distributing law and ore - controlling action about mouru ore belt. grasping distribution rule of the fractures in ore - forming zone by remote sensing analyse and field survey, and made a research about the ruptures " ore - containing character in the different orientation, putting forward that four ne - orientation structure containing - ore zone alternate with strong and feebleness

    論文詳細地論述了牟乳含礦帶的構造格局、斷裂分佈規律及控礦作用，通過遙感構造解譯和實地考察，從宏觀上整體把握了區域上和成礦帶內斷裂的分佈規律，對不同方向上斷裂的含礦性做了研究，並提出了牟乳礦帶內北東向的四個強弱構造含礦帶。
  9. Optimization of the productive prospect of the north ore belt at wushan copper mine

    武山銅礦北礦帶生產探礦的優化
  10. By researching geology condition and geology background, discourse thinks that tanlu rupture is mine - leading structure, the greater ne - orientation ruptures are ore - proportioning structure, sn - orientation ruptures are ore - containing structure in mouru ore belt

    結合膠東區域地質條件和地質背景，論文提出郯廬斷裂為牟乳金礦帶的導礦構造，一系列北東向的大型斷裂是配礦構造，而牟乳地區的北北東向斷裂只是容礦斷裂。
  11. Based on the study of geological, geophysical and geochemical characteristics of the background field, ore district and ore belt that the caijiaying ore deposit lies in, the authors have formulated the structural geological - geophysical - geochemical prospecting model, and summed up the optimum combinational process of geophysical and geochemical prospecting techniques

    摘要通過研究蔡家營礦床所處背景場、區域場、礦區、礦帶（床）等地質、地球物理、地球化學特徵，構建地質地球物理地球化學找礦模型，並總結出找礦勘查的物化探最佳方法組合流程。
  12. This paper has studied the ore - forming process of this ore belt and magmatic rocks, major vein rocks, wall rock alterations, trace elements and geochemical characteristics of various epochs, probed into the regularity of element enrichment and variation, and established geological - geochemical ore - prospecting criteria

    研究該礦帶成礦作用和在不同時代巖漿巖、主要脈巖、圍巖蝕變、微量元素及地球化學特徵， ?解元素富集變化規律，建立了地質地球化學找礦標志。
  13. Geological features and genesis for au deposits in the yangshan au ore belt, gansu

    甘肅省陽山金礦帶金礦成礦特徵及礦床成因研究
  14. Lying at the core part of qinling orogenic belt, the weishancheng au - ag polymetallic ore belt is a complex tectonic belt produced by repeated convergence, piecing together and welding of several strata and terrains which were formed in different tectonic settings and had their respective formation characteristics as well as independent deformation, metamorphic and tectonic evolutionary sequences

    摘要圍山城金銀多金屬成礦帶處于秦嶺造山帶東段核部，其由多個形成於不同構造環境，有著各自獨立的建造特徵、變形變質和構造演化序列的構造地層地體，經多次聚合后拼貼並焊結為一體的復雜構造帶。
  15. The mouping - rushan gold ore belt lies in the activated region on the eastern margin of the north china craton

    摘要山東牟乳金礦帶位於華北地臺東緣活化區。
  16. Principal compresso stress of mineralization epoch is measured 34 - 46ma by means of ae method, and its orientation is ew - trending by conjugate fracture, at last, the dynamic mechanics of the rhombic shear fault grid is analysised, ore - controlling law of the regional and ore - belt are determined, and combined with geophysical prospecting, ore - forming are forec ast

    利用巖石聲發射測得成礦期主壓應力值為34 - 46mpa ，以共軛破裂求得主壓應力方位為近ew向，分析了本區菱形剪切斷裂網格控礦構造應力場的動力學機制。提出區域和礦帶的成礦控礦規律，結合物探進行了成礦預測。
  17. Approach and analysis on ore genesis of no. 1 fe - cu ore belt in dahongshan iron ore deposit

    安徽省順風山鐵礦礦床地質特徵及成因分析
  18. According to the types of rock density and magnetism of magmatite, with separation, continuation, derivation, and false color encoding between gravity anomaly and magnetic anomaly as well as a composite process of their attributive information, the magmatite belts reflected by both gravity anomaly and magnetic anomaly can be divided into two belts and seven group sections based on their positions in the tectonic unit, the magma series characteristics, and the time - space relationship with the ore belt

    摘要根據不同類型巖漿巖的巖石密度、磁性的不同，通過重磁異常分離、延拓、求導、異常的彩色編碼及重、磁特徵信息的復合處理等，按重磁反映的巖漿巖帶所處的構造單元部位、巖漿系列特徵以及與礦帶的時空關系，將秦嶺造山帶劃分為2帶和7個群段。
  19. Isotopic geochemistry tracing for sources of ore - forming fluid in tianwan ore belt

    田灣金礦成礦帶成礦流體的同位素地球化學示蹤
  20. The complexity of ore - forming fluid isotopic composition in tianwan gold ore belt implies that the fluid was multi - source

    田灣金礦成礦帶中，成礦流體同位素組成的復雜性，反映了成礦流體是多源的。
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