ore bed 中文意思是什麼
ore bed
解釋
礦層-
When change cross fall and stroke still might maintain the surface of bed movement balance ； the spring lays aside in box in vivo ； the structure is compact, also it could obtain the final ore concentrate and the final debris onetime
在改變橫向坡度和沖程時仍可保持床面運行平衡，彈簧放置在箱體內，結構緊湊，且能一次得出最終精礦和最終尾礦。 -
The research for metallogenic evolution mechanism in the region indicates that gold ore formation has undergone three stages : gold elementary source bed formation stage from the neo - archean to the paleo - proterozoic and meso - proterozoic, regional metamorphism - migmatization gold reenrichment stage at the late meso - proterozoic, structure - fluid - gold mineralization stage at the yanshan period
對礦帶成礦演化機理的研究表明，金礦形成經歷了3個階段：新太古至古、中元古代金初始礦源層形成階段；中元古代末期區域變質混合巖化金再富集階段和燕山期構造流體金成礦作用階段。 -
Reduction in a mixed fluidized bed with iron ore and coal
礦煤混合流化床還原反應 -
From the characteristic of district gravity, the characteristic of remote sension. we can see that ore area develops south - north consotium rift. it not only controls the eastern edge of zhenxun basin, but also controls the form of bed
礦床類型以沉積、沉積?改造型為主。根據區域重力特徵、衛星影象和其他地質特徵，礦區所在部位，發育南北向的同生斷裂。 -
The places of gold ore is not only in the powerfulness place, but also in the place of tenacity - brittleness and the place of powerful deformation girdle place to the feeble the deformation in ductile zone gold bed
韌性剪切帶型金礦床中金的富集不僅在應變最強部位或韌性向脆性轉換的部位，還可以在強變形帶與弱變形域交接的部位。 -
Through the analysis of geological characters in huanglianken manganese ore district, such as ore potentiality, ore controlling structures, ore depositing structures, orebody characteristics, ore type and so on, the author concluded that sinian stratum is the " primary source bed ", detachment structure is the migrating channel of ore - forming materials, favorable concentration and hosting place
通過對黃連坑錳礦區地層的含礦性、控礦構造及容礦構造、礦體特徵、礦石類型等地質特徵的論述，認為震旦系地層是「初始礦源層」 ，滑脫構造對成礦物質起遷移、富集及容礦作用。 -
The genesis of spots in ore - bearing rock of baguamao gold deposit has been elaborated, through the geologic background, the characteristics of ore - bearing bed, the mutiperiodic mineralization and the mineral composition. the author indicates that the mottled structure of devonian system in qinling mts. resulted from the mutiperiodic activity of ore fluid and connected with the gold mineralization ， in addition ， it could be regarded as one of the important marks for gold mineralization
主要從成礦地質背景，含礦層特徵和多期成礦等方面闡述了八卦廟金礦含礦巖石中斑點的物質組成及其特徵，指出秦嶺泥盆紀含礦巖石中斑點狀構造為成礦流體多期作用的結果且與金礦化關系密切，可作為金礦化的重要標志之一。 -
Abstract : the genesis of spots in ore - bearing rock of baguamao gold deposit has been elaborated, through the geologic background, the characteristics of ore - bearing bed, the mutiperiodic mineralization and the mineral composition. the author indicates that the mottled structure of devonian system in qinling mts. resulted from the mutiperiodic activity of ore fluid and connected with the gold mineralization ， in addition ， it could be regarded as one of the important marks for gold mineralization
文摘:主要從成礦地質背景，含礦層特徵和多期成礦等方面闡述了八卦廟金礦含礦巖石中斑點的物質組成及其特徵，指出秦嶺泥盆紀含礦巖石中斑點狀構造為成礦流體多期作用的結果且與金礦化關系密切，可作為金礦化的重要標志之一。
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