associated ore 中文意思是什麼

associated ore 解釋
伴生礦石
  • associated : adj. 1. 聯合的。2. 聯想的。
  • 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。
  1. Finally, a review is made on the genetic relationships between mineralization and magma evolution and the associated characteristic of ore systems

    文中還介紹了層狀巖體中典型礦床的成礦作用與巖漿演化過程的成因聯系。
  2. Ore is normally associated with areas of high relief.

    在正常情況下,礦石與地勢高的地方有聯系。
  3. The design of ore dressing for the associated pyrity in mutimetal sulphide iron ore

    多金屬硫化礦中伴生硫鐵礦的選礦設計
  4. Ore minerals in the colorado-type deposits are of uraninite and coffinite, with associated vanadium and copper minerals.

    科羅拉多型礦床中的鈾礦物為晶質鈾礦和水硅鈾礦,與之共生的還有釩,銅礦物。
  5. 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
  6. Abstract : a separability study is conducted of pingle mine s grammite ore, which is associated with weakly - magnetic gangue minerals, such as mussite and garnet

    文摘:對伴生有透輝石、石榴子石等弱磁性脈石礦物的廣西平樂硅灰石礦進行了可選性研究。
  7. The wall rock of ore - bodies is the siliceous dolostone and alkaline volcanic rock ( trachy andesite ) in the yinachang deposit. based on the shape of ore - bodies and the structure and texture of ores, the deposit was identificed as synsedimentary with wall rocks. there occurred ree minerals, such as bastnaesite, monazite and allanite, associated with apatite and fluorite with ree contents to a certain extent

    礦體產出形態和礦石的結構構造等均顯示礦體與賦礦地層同沉積特徵;出現獨立礦物氟碳鈰礦、獨居石及褐簾石,磷灰石、螢石、菱鐵礦等礦物中也含有一定量的稀土,沿礦體走向和垂向稀土元素變化不大。
  8. Abstract : according to the variation in content of characteristic radioactive nuclide and the close relationship between high - grade associated elements in ore - forming components and gold, the ground gamma - ray spectrometry and x - ray fluorescence slectrometry can be used to reveal the existence of gold mineralization rapidly in field and make semi - quantitative evaluation of gold grade. this is of great significance in guiding field geological sample collection and mountain land engineering

    文摘:通過測定特徵放射性核素的含量變化以及利用成礦組分中一些高品位共生元素與金密切的相關關系,可利用地面伽馬能譜與x熒光測量在現場快速揭示金礦化的存在,同時對金的品位進行準定量評價,以及指導野外地質采樣和山地工程。
  9. According to the distribution features of vanadium, selenium, molybdenum and uranium at three interlayer oxidation zone tpye uranium deposits in northwestern china, their existence state and the mutual relation to uranium at known uranium deposits, it has been concluded that it is not sufficiently re - liable to make " spatial localization " of uranium ore bodies for interlayer oxidation type uranium deposits by prospecting the associated vanadium, selenium, molybdenum in soil

    根據我國西北業已查實的3個層間氧化帶砂巖型鈾礦床中釩、硒、鉬與鈾的展布特徵,認為,按已知鈾礦床中鈾與釩、硒、鋁的存在及相互關系,試圖用壤中釩、硒、鉬測量對層間氧化帶砂巖型鈾礦實施伴生元素找礦或進行「空間定位」的依據尚不足。
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