deposit region 中文意思是什麼

deposit region 解釋
存放區域
  • deposit : vt 1 放置，安置。2 使淤積，使沉澱。3 儲蓄。4 付保證金。5 寄存，委託保管。6 （把硬幣）放入（自動售...
  • region : n. 1. 地方，地域，地帶；地區；行政區，管轄區，區；左近，鄰近；（大氣、海水等的）層，界，境。2. 【解剖學；動物學】（身體的）局部，部位。3. （學問等的）范圍，領域。4. 〈罕用語〉天空。
  1. Origin and prospecting significance of guanyin temple lead - bearing black earth in the surrounding region of yongping copper deposit in jiangxi

    永平銅礦外圍觀音寺含鉛黑土成因探討及找礦意義
  2. That offer very valuable referential material for future searching mineral. in recent years, many deposits were confronted with reserves crisis in yuebei region. so we studied the typomorphic feature of pyrites, galenite, sphalerite for deposit of yuebei region, and sum up the genesis of deposit and mineral and reseaching typmorphic feature, these have important value to forecast the deepth of deposit and reaserch the outside of deposit

    近幾年，粵北地區的許多礦床面臨儲量危機，因而對粵北地區礦床黃鐵礦、方鉛礦、閃鋅礦的標型特徵進行研究，總結出凡口、紅巖、大寶山等礦床礦物的成因和找礦標型特徵，對于進行礦床的深部預測和外圍找礦工作具有十分重要的意義。
  3. Jadeite deposit in padaung region, burma

    古代玉符之說與翡翠早期應用歷史探討
  4. Grain - size characteristics and sedimentary environment in the lacustrian deposit of chaohu lake, the yangtze delta region

    長江下游巢湖湖泊沉積物的粒度特徵與沉積環境
  5. Setenaly according to the analyses from selected profiles, we know that, it is cold and dry in this region during the early holocene when east asian winter monsoon ' s influence is obvious, so, it is a transition period from sand deposit to sandy soil deposit, when the layers become thinner gradually from north to south. during middle holocene, it is warm and humid, influenced evidently by east asian summer monsoon, so, it is an obivious pedogenesis, when there are generally well - developped holecene palaeosol ( so ) from north to south, and the pedogenesis in the south is better than that in the north, the soil is also thicker than that of the north. from late holocene to now, the climate changes to be dry and cold, but its changing scope is smaller than that of last glacial period

    2 、就所選剖面分析來看，本區在全新世早期氣候回返，相對較寒冷乾燥，東亞冬季風影響較明顯，此時為沙層堆積向砂質土壤過渡，自北至南堆積的沙粒漸細；全新世中期氣候溫暖濕潤，東亞夏季風影響顯著，此時為明顯的成壤期，表現在自北至南普遍可見發育較好的黑壚土層，且南部的成壤作用比北部好，土壤的厚度也要大；全新世晚期至今，氣候向乾冷方向轉化，但變化幅度遠小於末次冰期。
  6. ( 7 ) showing and determining the evidence and timing of the lithophere delamination occurred in qinling orogenic belt. pointing out the gold deposit in xiaoqinling - xiongershan region are mostly formed during indosinian to early - yanshan movement, related to mantle fluid injecting caused by lithosphere delamination and plutonic activity caused by further large - scale tectonic extension

    初步闡述了東秦嶺地區的成礦分區和成礦特點，指出小秦嶺一熊耳山地區金礦形成的主要時期是印支一早燕山期，並且與巖石圈拆沉作用所引起的地慢流體活動和之後進一步大規模伸展作用產生的深源巖漿活動密切相關。
  7. Dongzigou ag deposit and jianbaoshan au deposit are hosted in the sandstone of middle - proterozoic suberathem, which are developed from the proterozoic sediment metal source - rocks formed during the meso - proterozoic volcanism and reworked by the mesozoic tectono - magmatism during the formation of the metamorphic core complexes in eastern hebei. the dongzigou ag deposit has the characteristics of reformed strata - bound origin, the jianbaoshan au deposit, located in the detachment fault, is the alterated rock type. both deposits have the similar wall - rock alteration, and show the same trace element behavior, and ree patterns. they are the results of the multi - stage tectono - magmatism in the environment of continental extension in eastern hebei region. their mineralization depended on their wall rocks and relative location in metamorphic core complexs

    賦存於中元古宙長城系常州溝組的洞子溝銀礦床和尖寶山金礦床是由密雲-都山變質核雜巖構造體系所控制的一組礦床。其成因為中元古宙火山巖漿活動形成的沉積礦源，后經中生代的變質核雜巖構造巖漿體系疊加改造而成。洞子溝銀礦床具有層控迭加改造的特點尖寶山金礦床則具有破碎蝕變巖型礦床的特點。
  8. By summarizing and analyzing the geological setting, uranium source, paleoclimate, hydrology, lithologic - lithofacies conditions in the region, it is indicated that the quantou formation in fanjiatun - jiutai area and the qingshankou formation in yangdachenzi area are potential metallogenic prospective areas for in - situ leachable sandstone type uranium deposit in the region, which develop braided channel or delta marginal sandstones, and possess favorable forming conditions of interlayer oxidation zone, and constituting supply - passage - discharge system of abundant uranium source

    綜合研究區域成礦地質背景、鈾源、古氣候、水文地質、巖性巖相條件，認為范家屯九臺一帶的泉頭組及楊大城子一帶的青山口組發育辮狀河或三角洲前緣砂體，構成了鈾源供應充足的補徑排系統，具有有利的層間氧化帶形成條件，是本區地浸砂巖型鈾礦的有利成礦遠景區帶。
  9. Circulation and ore controlling mechanism of sulfur and carbon in gold deposit accumulation region of eastern shandong

    膠東金礦集區硫和碳的循環與控礦作用
  10. They should remove the field plate and oxide and deposit a thin aluminum film over this region.

    他們應當去掉場極板和氧化層，並在整個區域淀積一層薄的鋁薄膜。
  11. There are plentiful mineral resources of nickel, cobalt, and copper in the northwest region of china, specially jinchuan superlarge copper - nickel sulflde magmatic deposit in gansu province, known for its large scale and typical metallogenetic feature in the world, is an important source of ni - cu metal mineral resource in our country. in contrast, jianchaling large cobalt - bearing nickel sulflde deposit in shannxi province is not famous and unmined, but many problems about the deposit are researched because of its special geologic settings and mineralization characteristic

    我國西北地區有著豐富的鎳、鈷、銅等金屬的礦產資源，尤其是甘肅省金川超大型銅鎳硫化物巖漿礦床，以其超大規模及其典型的成礦特徵而聞名於世，是我國重要的鎳、銅金屬礦產基地，而相比之下，陜西省煎茶嶺大型鎳（鈷）礦床規模較小且未開采，但因其獨特的地質背景和成礦特徵而具有重要的研究意義。
  12. Baibao area lies in the middle - south of the basin, delta deposit was belong to the north set of jingbian - wuqi delta and locating at front region

    白豹地區位於盆地中南部，三角洲沉積屬于北部靖邊?吳旗三角洲向西南延伸部分，主要發育三角洲前緣沉積。
  13. By applying the theory and method of geological anomaly, it is focused on the analysis of the characters of major geological anomalies and their effect of mineralization in daye - jiurui region. the analysis result shows that the basement fault anomalies control a few major large hidden batholiths and their associated orefields ; that the anomalies of cover structure confine most cu - au deposits and fe - cu deposits within their scope ; that the geochemical anomalies and lithofacies - paleogeographical anomalies are major geological factors leading to trataboundness of some cu - au deposits ; that the anomalies of rock operties provide the favorable chemical and physical conditions for the ore - forming process, including the seepage, circulation, convergence and deposit of ore - bearing hydrothermal solution ; that the anomalous ctive stage of mesozoic magmatite is almost consistent with the major mineralization epoch of the fe, cu deposits, and the structure of multi - levels, and the zoning in magmatic system determine the spatial distribution of the mineralization system. then, based on the above analysis, a comprehensive variate, geological combination entropy, is brought forward for reflecting the complex degree of the combination of geological ore - controlling factors. after circumscribing the anomalies of geological combination entropy, the relations between the anomalies and ore deposits are determined

    從地質異常的角度，重點分析了大冶九瑞地區主要地質異常的特徵及其對成礦的影響.由分析可知：基底斷裂異常控制了本區若干重要規模較大的隱伏巖基及伴生礦田，而蓋層構造異常控制銅金礦床和鐵銅礦床的空間位置；地層的地球化學異常和巖相古地理異常是造成一些銅金礦床層控性的主要地質因素；蓋層的巖性異常為含礦熱液的滲流、循環、聚集和礦質沉澱等一系列成礦作用提供了有利的物理和化學條件；中生代巖漿巖的異常活動期也是本區主要的鐵銅成礦期，巖漿巖系統的多層分枝和分帶性結構控制了本區成礦系統的三維空間分佈.在上述分析的基礎上，構置了地質組合熵作為反映控礦地質因素組合系統結構復雜程度的綜合變量，並圈定出組合熵異常，由此確定了綜合地質異常與礦床的關系
  14. The prospecting for panhudu cu - au deposit in jiurui region, jiangxi province

    江西九瑞地區潘湖渡隱伏銅金礦找礦前景
  15. Dongxiang copper deposit is located at the transition zone between cathaysia and jiangnan terrains, which is geotectonically included in jiangxi - guangxi diwa system, southeast diwa region. dongxiang copper deposit is a part of northeast jiangxi colored - metal zone

    東鄉銅礦位於江南地體與華夏地體的交接部位，在大地構造位置上屬于東南地窪區的贛桂地窪系，是贛東北有色金屬成礦帶的一部分。
  16. The midland region of china includes eight provinces, which has abundant energy deposit such as coal, oil and water power

    摘要中部地區煤炭、石油和水能資源的稟賦較高，但是各個省份的能源狀況差別很大。
  17. Why do such a new system give much help in poverty reduction in the developing countries ? this paper give us some new advice on micro - credit of our country by discussing the development processes of micro - credit worldwide and the practice of our country : 1 、 our institution of micro - credit should find enough public capital to make it better than the traditional institution that only relying on the state finance or donative capital, in one word, there is about 950 billion $ underground in our country. we should manage to attract so these capital to attend in poverty reduction, in another word, much capital that deposit in the post saving institution and the rural credit institution have outflow away the rural region because of lacking of investing channels

    本文主要在考察世界范圍內小額信貸的產生與發展過程，並從中汲取經驗，結合我國小額信貸的運作實踐，為我國的小額信貸的進一步擴展提出了一些新的看法:我國小額信貸必須突破現有的依靠捐助資金或財政補貼運作的單一資金渠道來源的運作方式，想方設法從民間獲得機構持續發展的必需資金，在我國，一方面存在著大量的地下金融活動，約有大約9500億元的資金，這是我們可以動員的資金，使它們參與到小額信貸中來，而另一方面，在我國由於缺乏正規的投資渠道，才會有如此巨大的資金存在於正規金融體制之外，而且，我國農村正規金融機構農村信用社，從農村吸收的儲蓄存款，由於難以在農村尋找合適的信貸項目，大量資金流出農村，郵政儲蓄機構同樣存在這樣的情況，這些都是農村發展中的資金瓶頸形成的因素。
  18. The sublacustrine fan, as an important deposit in actic region of northern chexi sub - sag, is characterized with both source and reservoir in it and favorable hydrocarbon accumulation conditions

    摘要湖底扇是車西窪陷北部陡坡帶的一種重要的沉積類型，具有自生、自儲的特點，成藏條件優越。
  19. The paper analyzed sedimentary characteristics and depositional environment in t1f3 this region firstly, and on the grounds of establishing logical deposit pattern gave emphasis to make a study of distributing laws and spreading traits of the oolitic beach. because diagenesis is a vitally dominating factor that influenced oolitic beach reservoir nature in the region, the master diagenetic events of the reservoir in the lengthy geological history, as well as the influence to the pore abundance, was made a study of. the diagenetic stages and sequences were divided and the pore evolve pattern was established in the paper

    本論文首先分析了研究區飛三段的沉積特徵與沉積環境，在合理建立沉積相模式的基礎上重點研究了鮞粒灘（壩）的分佈規律和空間展布特點；成巖作用是影響本區鮞灘儲集性至關重要的控制因素，論文詳細研究了儲層在漫長地質歷史過程中所經歷的主要成巖事件及其對孔隙發育的影響，劃分了成巖階段與成巖演化次序，建立了孔隙演化模式並以建南構造為例進行了成巖相展布研究的嘗試；最後還在鮞灘儲層基本特徵研究的基礎上對飛三段儲層進行綜合評價與預測。
  20. The geological structure and cu deposit explored and new information of geochemistry related to cu deposit show that there are huge potentials for prospecting cu deposit in this region

    筆者經綜合研究地質構造、銅礦勘查及有關地球化學等新信息后，均顯示出巨大的銅礦找礦潛力。
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