sub ore 中文意思是什麼
sub ore
解釋
次級礦石-
The ore - forming material is mostly from volcanic rock, and sub volcanic rock provides the main thermal and some mineral materials. the ore - forming fluid is from meteoric water. as a result, it should be a kind of adularia - sericite type of epithermal gold deposit
成礦物質主要來自礦區火山巖圍巖，次火山巖提供了主要熱源和部分礦源，成礦流體來自大氣降水，礦床成因類型為低硫化物冰長石?絹雲母型淺成低溫熱液型金礦。 -
The minerogenetic model of xikuangshan type copper deposit can be concluded that : in jinningian - chengjiangian, the activity of xiaojiang discordogenic fault form dextrorotation sub - structure in dongchuan ore area
昆陽裂谷內的多數銅礦同位素成礦年齡多集中在9 . 0億6 . 5億年之間，屬于晉寧-澄江期，與rodina大陸裂解時限相當。 -
Deep and sub fissures were advantageous fields for ascending and assembling of the ore - forming thermal fluid. in addition, gritstone and mudstone provided the condition for the atmospheric water ' s descending
深大斷裂及次級斷裂是深部成礦熱液上升和匯集的優良場所，周圍砂巖和泥巖又為大氣降水的滲透提供了條件。 -
Based on ore material sources, metallogenesis, occurrences, ore formation and wall rock alteration of gold ore deposits in the northest jiangxi province they are classified into four types i. e. magmatic hydrothermal gold deposit, volcao - subvolcano hydrothermal gold deposit, multi - sources hydrothermal gold deposit and heat underground water ( brine ) infiltrating gold deposit and 8 sub - types and the geological characteristics of the deposits are described and ore - forming control of sedimentary formation, structure and magmatic rocks on the formation of gold ore are summarized and gold ore - searching directions in the northeast jiangxi province are pointed out
依據成礦物質來源、成礦作用、礦床產出條件、礦石建造和圍巖蝕變等因素，將贛東北地區巖金礦床劃分為巖漿熱液類、火山次火山熱液類、多源熱液類和地下熱（鹵）水滲濾類等4類8型，分述了各類（型）金礦成礦地質特徵，總結了沉積建造、構造和巖漿巖對區內金礦的控製作用，指出了贛東北地區金礦找礦方向。 -
Ore bodies, sub - marginal economic resources, marginal economic reserves and economic reserves can be contoured respectively with the former three
利用前3項品位指標可以分別圈定礦體邊界、次邊際的資源量、邊際經濟的儲量、經濟儲量。 -
In high mountain distribute on the this and hetian jade catch mineral deposit and ore order, many river return output and sub jade, hetian jade originally
在高山這上分佈著和闐玉的原生礦床及礦點，不少河流中還產出和闐玉的子玉。 -
In this paper, with the metallogenic series theory as the guide and the geochemical data as the basis, all lead - zinc ore deposits in the region were classified into two sub - series, i. e., lf type ( with low content of iron group elements ) and hf type ( with high content of iron group elements ), and a regional geochemical prognostic model was set up by using the logical information method
摘要以成礦系列理論為指導，將區域內的鉛鋅礦按地球化學特徵劃分為貧鐵型和富鐵型2個亞系列，進而用邏輯信息法建立了西秦嶺鉛鋅礦床區域地球化學場預測模式，驗證結果較為理想。 -
The famous jade pit was as follows, in the past qi house hole whether lie in field agate jade ore then, i of county, the people build by qi house brother ore exploit the beginning latter stage of qing dynasty, yang of hole at i agate ore then too, card qiang hole don t mountain material not made in county, in addition, and the tower stone stockaded village of black hills of field produces the sub jade
以往著名的玉礦坑有：戚家坑在於田縣阿拉瑪斯玉礦，清末民初由戚家兄弟建礦開采，楊家坑也在阿拉瑪斯礦，卡羌坑且末縣出產的山料，此外，和田黑山塔石寨產子玉。 -
The explanation proposed by this paper is that, the mineral sequence in the mineralization is decided by the differentiation of ore - forming fuid system and the orderly deposition of each sub - system derived from the differentiation
本文認為最佳的解釋是，成礦流體體系的分異及其分異出來的各個子體系有序的賦存層次決定了成礦階段的有序性。 -
The source of gold ore is actually an ore - forming fluid storeroom, in which the sub - systems of ore - bearing solution with various properties occur in different levels in the course of migration, differentiation and convergence
因此，提出了金的液體礦源是通過運移分異作用成礦流體的匯聚過程，並構成了不同性狀的含礦流體的子體系分層次賦存的成礦流體庫。
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