minerogenetic 中文意思是什麼
minerogenetic
解釋
成礦的-
Analysis on the minerogenetic geological condition of the gold ore in the lianhuashan anticline, western guizhou
貴州蓮花山背斜金的成礦地質條件分析 -
Article 24 in conducting a general survey of mineral resources, after completing survey of the major minerals, a preliminary comprehensive assessment shall be made of the minerogenetic conditions involving all paragenetic or associated minerals and of the industrial perspective of the mineral deposits in the area being surveyed
第二十四條礦產資源普查在完成主要礦種普查任務的同時，應當對工作區內包括共生或者伴生礦產的成礦地質條件和礦床工業遠景作出初步綜合評價。 -
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。 -
The axi gold deposit ; laumontitization ; epithermal gold deposit ; geothermal fluid minerogenetic system ; west tianshan
阿希金礦濁沸石化淺成低溫熱液型金礦地熱流體成礦系統西天山 -
( 4 ) through level division of the predict result which favorable for mineralize district in the studied areas. we put up a graduate method which is used to divide graduations of statistical result. this kind of dividing method is different from traditional interval or non - interval graduate method, it can avoid a subjectivity for level division and is favorable to divide the high value of the result. ( 5 ) in the light of rank points and weight of the predicting factors, minerogenetic prediction map had been made. on the basis of the map, six favorable districts to mineralize had been determined
這種劃分方法不同於傳統的等間距、不等間距劃分方法，避免了劃分的主觀性，更有利於對預測結果高值區域的劃分； （ 5 ）根據預測因子的級別分數和權重，通過gis疊加分析操作，生成一系列的成礦預測系列圖件，根據預測圖件，在研究區圈定6個成礦有利區。 -
The efficiency and reliability of minerogenetic prediction can be improved by combining rs with gis. we processed rs images, extracted the geological information related to mineralizing, such as geology, structures, stratam, rocks, etc, synthetically analysed remote sensing, the geological data and geo - chemistry, under the guidance of the theory and mathematic model, set up gis mineralize model. on this condition, to develop this method and its theory, and to establish a system of perfect prediction, it is not only useful in studied degree area but also favorable for looking for new type and some form large - scale deposits in old studied area, and it has a great theoretical meaning
遙感與gis相結合用於成礦預測中可大大提高預測工作的效率和可靠性。通過對研究區的遙感圖像處理和地質、構造、地層、巖石、礦化蝕變等有關信息的特徵提取、遙感、地質數據和物化探數據的綜合與復合分析，在一定成礦理論和數學模型指導下，建立gis綜合找礦模型。在此基礎上，發展這一方法及理論並建立完善的預測體系，不僅對研究程度較低的新區礦床預測有用，而且對研究程度較高的老區尋找新類型和點狀大型、超大型礦床都具有重要理論意義和實際意義。 -
Basing on the above research and fully using geologic, geophysical, geochemical and remote - sensing etc. data, the author determines seven order iv metallogenic provinces and seventeen order v metallogenic provinces in fujian and discusses the minerogenetic geologic characteristics and gold - finding direction of the four important order iv metallogenic provinces ( jianning - taining, youxi - dehua, zhenghe - jianou and jianyang changping - dajinshan ). all the order v metallogenic provinces are classified and the their geologic features and main gold - prospecting categories are briefly introduced
對省內四處重要的金礦級成礦遠景區（建寧?泰寧、尤溪?德化?永泰、政和?建甌、建陽長坪?大金山）的成礦特徵及找礦方向進行了探索，對級成礦遠景區進行分類，並概述了各成礦遠景區的特徵和找礦主攻類型。 -
Alkali basite, which came from upper mantle or lower crust, invaded through those structure, which not only bring cu et al mineralizing elements, but also the most important is that thermal energy. it cycled the formation water ( yinmin fonnation and luoxue formation ), and form alkali - rich, middle - high temperature and salinity fluid mixed with alkali - rich magmatic water. there were high rate of percolation and well voidage in the contact zone between yinmin purple stratum and yinmin rubblerocks, which is in favor of the transposition and mineralization of minerogenetic fluids
因此，總結東川稀礦山式銅礦成礦模式為沉積（ fe 、 cu ） ?熱液疊加（ cu ）改造：晉寧-澄江期，小江深大斷裂發生走滑運動，在東川礦區造成右行旋扭及其派生構造，形成「 z 」字形落因破碎帶，同時來自深源（下地殼或上地幔）堿基性巖漿侵入，不僅帶來了大量cu等成礦物質，更重要的是提供了熱源，促使地層水（落雪組白雲巖和因民組紫色層）循環，與富堿（ na和k ）巖漿水混合，形成富堿中高溫高鹽度流體。 -
D ) the invasion of jinningian - chengjiangian alkali basite were unambiguous, the distribution of those rocks form " z " in shape, which similar with luoyin fracture zone and the distribution of copper deposit. it shows that copper deposits were controlled by discordogenic fault and its derived sub - structure, and there are relationship between copper deposit and jinningian - chengjiangian alkali basite. e ) most of minerogenetic age of copper deposit, which located in kunyang rift valley, belongs to jinningian - chengjiangian ( between 900 - 650ma ), similar with the time limit of breaking - up of rodinia
東川礦區晉寧-澄江期堿基性巖侵入活動明顯，常作為因民組復雜角礫巖膠結物和巖脈（體）產出，多分佈於深大斷裂及其派生的次級構造附近，明顯受南北向小江深大斷裂走滑運動引起的右行旋扭及其派生構造控制，與「落因破碎帶」和「銅礦分佈」較吻合，均為「 z 」字形。 -
By study dabaoshan deposit on minerogenetic and geological background, mineral constituent, rare - earth element, isotope and typomorphic feature of sulpurization mineral, finally, we made a conclusion that dabaoshan deposit resulted from the volcanic deposition which type is laterebuilt and magma hydrothermal superimposed. we found the upside of dabaoshan deposit have been denuded or oxidized, bassically, it have reached the lowest part of the deposit
通過對大寶山礦床的成礦地質背景、礦物成分、稀土元素組成、同位素以及黃鐵礦、閃鋅礦、方鉛礦的標型特徵進行研究，確定了大寶山礦床的成因為火山沉積，經後期巖漿熱液疊加型礦床，對礦床的遠景進行了預測，提出大寶山礦床的上部礦體已被剝蝕或被氧化，基本上已經到礦體的深部的觀點。 -
The following new knowledge are acquired : a ) the cu background of stratum and jinningian alkali basite is abnormal high, which could be liberated from those rocks during alteration. cu et al. minerogenetic elements, which main came from magmatic rock, some from stratum ( yinmin formation and luoxue formation ) and its basement rocks
礦床中cu等成礦物質來源復雜，以深源為主，部分來源於地層（因民組紫色層和落雪組白雲巖）及基底地層；礦區內的退色蝕變作用可能是混合流體堿質交代改造作用的結果，對銅礦形成影響明顯，是銅礦化的標志； 2 -
The minerogenetic epoch lasted from paleoarchean to sinian, with neoarchean, paleoproterozoic and mesoproterozoic - qingbaikouan being the culmination periods
成礦時代從古太古代到震旦紀，但以新太古代、古元古代、中元古代青白口紀3個地質時期為成礦高峰期。 -
90 ' s it was found in shizishan, yimen, indicated that the type deposit is well explorative prospect in dongchuan - yinmen. by sum up the data of trace elements, isotopic elements, fluid inclusions and minerogenetic age et al.,
稀礦山式銅礦以落雪礦區稀礦山礦段最為典型，主要分佈在因民落雪大喬地?稀礦山、濫山、磨子山，濫泥坪6 ? 4巷、白錫臘和拖布卡地區。 -
Preliminary study on the minerogenetic model of mesozoic volcanic - magmatic rocks in eastern jilin, china
雲南斷陷盆地淺循環巖溶水賦存規律初步研究 -
The preliminary study of laumontitization of axi gold deposit and paleogeothermal minerogenetic fluid system in west tianshan
西天山阿希金礦濁沸石化與古地熱成礦流體系統的初步研究 -
Cu et al minerogenetic elements were liberated from stratum by the affection of the mixed fluid, overprinted and alternated the original mineralization, and form xikuangshan type copper deposit
在這種混合流體作用下，地層中cu等成礦物質析出，疊加改造了初始銅礦化，最終形成稀礦山式銅礦。 -
With the geological evolution in precambrian, minerogenetic materials and types of mineral deposits obviously varied and increased
隨著中國前寒武紀地史的演化，成礦物質種類和礦床類型具有明顯的變化和增多。 -
The preliminary study of laumontitization of axi gold deposit and paleogeothermal minerogenetic fluid system in west tianshan bao jingxin chen yanjing zhang zengjie chen huayong liu yulin
鮑景新，陳衍景，張增傑，陳華勇，劉玉琳 -
Minerogenetic mechanism and condition of wulong gou gold deposit in east kunlun mountains, qinghai province
青海東昆侖五龍溝金礦床成礦條件及成礦機理 -
By analyzing and generalizing minerogenetic and geological background, mineral constituent, rare - earth element, isotope and typomorphic feature of sulpurization mineral, finally, we made a conclusion that fankou desposit resulted from the hot spring eruption at the bottom of sea, it has a character of syngenetic sedimentary deposit, which was affected by the late hydrothermal superimposed and light rebuilding after it came into being, which is typical sedex bedded - controlled deposit
通過對凡口礦床的成礦地質背景、礦物成分、稀土元素、同位素以及的黃鐵礦、閃鋅礦、方鉛礦標型特徵進行了分析總結，確定了凡口礦床是海底熱泉噴溢形成的，同時又受到後期熱液輕微疊加改造，屬于典型的sedex型層控礦床。
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