金屬礦帶 的英文怎麼說
中文拼音 [jīnzhǔkuàngdài]
金屬礦帶
英文
metal zone-
In the baggage cars, kelps, fishplate, rolled iron, sleepers, wire rods, plates and sheets, laminated articles, hot rolled hoops, splints and mortar carriages, and zor s ore
車里裝著海帶、魚尾板、鋼材、枕木、盤鋼、厚金屬板、疊合材料、熱軋鋼箍、軟木條和迫擊炮車，以及佐澤斯礦石。( 6 ) the geological significance of oblique - thrusting fault of sertengshan - xitieshan was discussed in this paper. the oblique - thrusting effect of sertengshan - xitieshan is the result of the long distance effction of himalayan orogenic belt intracontinent subducting, which is of great theory significance for studying regional structural framwork, relations between basins and mountains and oblique - thrusting effect of large - scale fault zone or orogen in northern qaidam basin. moreover, the result is of guidance significance for the forecast of combination gas, distributing and formation of nappe metal deposit in northern qaidam basin
（ 6 ）論文探討了賽什騰? ?錫鐵山斜向逆沖推覆構造的地質意義，認為賽什騰-錫鐵山斷裂斜沖作用是印度板塊與歐亞板塊碰撞、會聚的遠程效應的結果，該認識對于研究柴北緣區域構造格局、盆山關系以及更大尺度的斷裂帶或造山帶的斜向逆沖作用具有理論意義，對柴達木北緣的油氣預測、推覆體金屬礦床的分佈、形成具有指導意義。Epithermal au - ag polymetallic deposit in western sichuan province
南角河銀多金屬礦床的垂直分帶特徵Chener gold deposit is located in north of xunmadao fault, the types of ore are gold - brazil - quartz of vein and gold - multimetal - quartz of vein. the occurrence of gold - bearing quartz vein is controlled by ductile - brittle shear zone, most the occurrence of gold - bearing quartz vein included by schistous zone and cracked zone, in the strike direction of gold - bearing quartz vein, it " s high content and great thickness appear on nww, in the direction of tilt, it " s high content and great thickness appear on the part of transformation from big angel of tilt to small angel of tilt
礦石類型為金-黃鐵礦-脈石英型和金-多金屬硫化物-脈石英型。含金石英脈受韌-脆性剪切帶控制，主要賦存於片理化帶與破碎帶中。在脈體走向上，北西西向脈體品位高，礦體厚度大；在傾向上，南傾，傾角較緩處品位高、礦體厚度大。Major product has crane and mine to use related service and the products such as exavator, the rolling mill of seamless steel tube, board tape rolling mill, the oil membrane bearing of rolling mill, the extruder of nonferrous metal, forging press, burnt stove equipment, pressure vessel, deceleration machine, train axle, train ship, precise casting forging and large scale casting forging
主要產品有起重機、礦用挖掘機、無縫鋼管軋機、板帶軋機、軋機油膜軸承、有色金屬擠壓機、鍛造壓機、焦爐設備、壓力容器、減速機、火車軸、火車輪、精密鑄鍛件、大型鑄鍛件等產品和相關服務。There are a series of lead - zinc polymetallic deposits, such as fozichong, dongtao, xiashui, wenlongjing and jilongding distributed along the fault zone. these deposits have some similiar features : ? ll of them are bounded in the strata of lower palaeozoic group ; ? ain orebodies occur as stratiform or stratoid form with occurrence consistent with that of host strata ; ? tratiform skam or baritic rock are the direct country rock of orebodies ; ? ypical syngenetic sedimentary fabric preserved in the ore. these deposits may be included in the same metallogenic series
佛子沖、東桃、下水、文龍徑、雞籠頂等一系列鉛鋅多金屬礦床沿該斷裂帶分佈，這些礦床雖然在成礦規模、賦礦層位和礦石礦物組成等方面存在一些差異，但均產于下古生界地層中；主要礦體呈層狀、似層狀產出，與地層產狀大體一致；直接賦礦圍巖為層狀綠色巖或重晶石巖；礦石中保留有典型的同生沉積組構。Other bound metals related to iron - manganese oxides and silicate indicate no change above the loess covered deposits
鐵錳氧化物態硅酸鹽結合態金屬元素在厚黃土覆蓋區對礦帶無指示意義。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。( 8 ) suggesting the deposit information in central south part of xingan - mongolia orogenic belt relate to the two events of mantle upwell and lithosphere extension since late - paleozoic. first is the lithosphere de
在這些中酸型小巖體與早二迭系地層的內外接觸帶往往形成eu 、 pb 、 zn 、 sn 、 ag 、 au等多金屬礦床和礦化密集區。Yuebei region is one of the important mineralized zone of nonferrous metal and sulphur in china
粵北地區是我國有色金屬及硫的重要礦化帶之一。Nanning is located lingnan nonferrous metal bands, underground mineral - rich, the survey found there is manganese, aluminum, gold, silver, quartz sand, crystal, dolomite, 4 1 species ; wildlife, especially chinese herbal medicine resources, very rich
南寧地處嶺南有色金屬帶，地下礦藏豐富，現已勘查發現的有錳、鋁、金、銀、石英砂、水晶、白雲石等41種；動植物，尤其是中草藥資源，十分豐富。On it ' s way back up, it then carries the gold atoms along with it and when the high pressures and temperatures decrease, the gold condenses into veins of pure metal
當流水返回時便攜帶著金原子，一旦高溫、高壓開始減弱金就會以純金屬的方式濃縮在礦脈里。Throughout researching it has been found that three main types of copper deposits, which mafic - ultramafic rock, marine volcanic rock and porphyry, with middle proterozoic, paleozoic and mesozoic in gansu, china. the cu - bearing formation, deep major faults and late structural - magmatic zones formed in specific geotectonic setting are main ore - controlling and metallogenic factors for copper, gold and polymetallic minerals in this area, and their convergent positions are effective ones formed ore bodies in space
通過研究認為：鎂鐵質-超鎂鐵質巖型、海相火山巖型及斑巖型三種銅礦類型，是甘肅的主要銅成礦類型，其主成礦階段為中元古代、古生代以及中生代；特定大地構造背景下形成的含礦建造、區域性深大斷裂以及後期斜向構造-巖漿活動帶，是該區銅、金及多金屬成礦的主要控礦因素，三者在空間上的復合是礦床體形成的有利部位。Northern three - river metallogenic belt is one of the most important nor - ferrous metal metallogenic belts in our country. reserves of cu, pb, zn, ag are very large. the area locates in arc bend of himalayan tectonic region, and is of unique tectonic character
西南三江北段成礦帶是我國最重要的有色金屬成礦帶之一， cu 、 pb 、 zn 、 ag儲量豐富，並且地處喜馬拉雅構造域的弧形拐彎地段，構造位置獨特。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。The north - eastern structural zones which become intensity from the western part to the eastern one in gansu show a influence of marginal - west pacific indosinian - yanshan tectonic - magmatic belt on the western part of china ' s continent, and not only a important regional metallization had developed but also early - formed minerals were intense changed and enriched with the tectonic - magmatic activity
甘肅境內由西向東增強的北東向構造帶，是我國東部濱西太平洋印支-燕山期構造巖漿活動帶向大陸西部的延伸表現；伴隨該期構造-巖漿活動，區內發生了重要的區域性成礦作用，並使處于該期構造活動帶的先期金屬礦產遭受了較強的疊加與再生改造。Based on geological and geochemical exploration data of more than twenty copper and polymetallic deposits, including data of regional geology, ore belts ( orefields ) and ore deposits on different scales, the authors put forward the geochemical method for quantified appraisal of anomalies in large deposits
摘要集20多個銅、多金屬礦床的區域、礦帶（田） 、礦床不同比例尺的地質、地球化學勘查資料，研製了定量評價大礦異常的地球化學方法。Xikuangshan type copper ore deposit named those fe - cu deposits hosted in yinmin formation, kunyang group, which located in kunyang rift valley and the edge of southwest yangzi platform. the best example is xikuangshan allotment, luoxue ore area, dongchuan, yunnan. the type deposit spread in south kunyang rift valley, include dongchuan, wuding - luoci, yuanjiang, yimen, huashengping, hongmenchang and so on
稀礦山式銅礦是指賦存在昆陽群因民組地層中的銅鐵礦床，其大地構造背景屬于元古代裂谷帶，大陸裂谷是超大型銅等多金屬礦形成和分佈的有利環境，在裂谷下部常發育異常地幔和巖漿源，裂谷空間上的多層次性使礦床具有明顯垂向分帶特徵，其演化時間的長期性、脈動性和繼承性便於多期成礦作用相互疊加、礦質的高度聚集。Geological, geophysical and geochemical research indicate that ore deposits space distribution present belt in nw direction and strip in ne direction is controlled by the lengthwise structure and transversal structure. in the fold - thrust belt, those ore deposits formed in pre - intracontinental - orogenic stage, such as dingqinnong ag - cu polymetal ore deposit, have the character of one orebody beneath one, so it is optimistic to search new orebodys in deep
地質、地球物理、地球化學研究表明江達構造帶礦床在空間上呈現北西成帶、北東成條規律分佈受縱向構造與橫向構造的雙重控制；在褶皺?沖斷帶，陸內造山期之前形成的礦床（如丁欽弄銀銅多金屬礦床） ，常出現礦體多層疊置、礦下有礦的現象，深部找礦前景樂觀。Continent block colliding during late - permian to middle - triassic ; lower part delamination and upper part rifting of lithosphere during late - triassic ; delayed compression and uplift during early - jurassic ; crust extension from middle - jurassic to early - cretaceous ; large - scale strike sliping from late - cretacoues to present. ( 6 ) roughly expounding the deposits distribution feature in south part of sanjiang orogenic belts, especially in detail to set forth the characters of southern nanchangjiang cu, pb, zn, ag, sn, fe metallogenic belt
初步闡明了三江造山帶南段礦床的時空分佈特徵，特別是較系統闡述了與巖石圈拆沉作用相關的南瀾滄江cu 、 pb 、 zn 、 ag 、 sn 、 fe成礦帶的特點，指出含鉀較高的火山巖可作為尋找拆沉環境中銅多金屬礦的有利地區，而火山巖中孔隙度較高的層位、層面和破碎帶可作為優先找礦部位。分享友人