火成變質巖 的英文怎麼說

中文拼音 [huǒchéngbiànzhíyán]
火成變質巖 英文
orthorock
  • : fire
  • : Ⅰ動詞1 (完成; 成功) accomplish; succeed 2 (成為; 變為) become; turn into 3 (成全) help comp...
  • : Ⅰ名詞1 (性質; 本質) nature; character; essence 2 (質量) quality 3 (物質) matter; substance;...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  1. In spatial distribution, coal fields are developed in the anomalies of high chargeability sedimentary areas ; metamorphic iron deposits occur in the anomalies of high chargeability metamorphic areas ; endogenic gold deposits are found in the anomalies of high chargeability igneous areas

    空間分佈上,與沈積作用密切相關的煤礦主要分佈在沈積高極化率地區,鐵礦主要分佈在高極化率地區,內生金礦則主要分佈在高極化率地區。
  2. The feldspathic sandstones belong to this formation of composite sources metamorphic, sedimentary, and igneous sources, but mainly from metamorphic source due to the high abundance of brown cl colors of quartz

    上述情況表明,研究區長石砂物源母包括、沉積,但從發育大量棕色石英顆粒來看,物源以為主。
  3. After making detailed research on ore - controlling factors, the author points out that gold deposits in fujian resulted from the various geologic processes such as sedimentation, metamorphism, tectonism and magmatism

    詳細研究了福建省金礦的金礦的控礦因素,提出省內金礦的形是沉積作用、作用、構造作用和漿作用(包括山作用)的綜合結果。
  4. Dongzigou ag deposit and jianbaoshan au deposit are hosted in the sandstone of middle - proterozoic suberathem, which are developed from the proterozoic sediment metal source - rocks formed during the meso - proterozoic volcanism and reworked by the mesozoic tectono - magmatism during the formation of the metamorphic core complexes in eastern hebei. the dongzigou ag deposit has the characteristics of reformed strata - bound origin, the jianbaoshan au deposit, located in the detachment fault, is the alterated rock type. both deposits have the similar wall - rock alteration, and show the same trace element behavior, and ree patterns. they are the results of the multi - stage tectono - magmatism in the environment of continental extension in eastern hebei region. their mineralization depended on their wall rocks and relative location in metamorphic core complexs

    賦存於中元古宙長城系常州溝組的洞子溝銀礦床和尖寶山金礦床是由密雲-都山核雜構造體系所控制的一組礦床。其因為中元古宙漿活動形的沉積礦源,后經中生代的核雜構造漿體系疊加改造而。洞子溝銀礦床具有層控迭加改造的特點尖寶山金礦床則具有破碎蝕型礦床的特點。
  5. Abstract : to the principle and project that tu guangazhi proposed in 1990, the gold ore deposits in qinling ( shaanxi ) may be classified into fouowing types : archean high - grade gneiss type, fine grained fragmental rock - carbonate rock - silicilith type, metamorphic fragmental rock type, volcanic rock type, explosive breccia type, intrusive rock exo - and endo - contact zone type. inthis paper, the geological characteristics, metallogenic geological setting, the source of ore - forming materials, digenic mechanism and metallogenetic epoch of gold ore deposits are also discussed

    文摘:參照塗光熾先生( 1990 )提出的礦床類型劃分原則與金礦分類方案,將陜西秦嶺地區原生金礦劃分為太古界綠建造型、細碎屑-碳酸鹽-硅建造型、碎屑型、建造型、隱爆角礫型和侵入內外接觸型金礦,並對各類型金礦的地特徵、礦地背景、礦物來源、礦床形機制及形時代等問題進行了論述和討論。
  6. By the study of metallogenic geologic characteristics of the various gold deposits, the author sets up the ore - forming model of some typical deposits such as shuangqishan deposit and zhijinshan deposit etc. it is considered that the gold deposits of metamorphic rock category and the volcanic rock category are the main gold - prospecting categories and carlin gold deposit and mulongtao gold deposit are the potential categories in fujian province

    系統總結了福建省各類型金礦的礦地特徵,建立了雙旗山金礦和紫金山銅金礦等典型礦床的礦模式,提出了型金礦和型金礦是福建省金礦找礦的主攻類型,卡林型金礦和穆龍套式金礦為潛在找礦類型。
  7. The main achievements obtained in this paper are as follows : 1. some of new recognitions were obtained on such aspects as strata sequence, rock type, metamorphism, hydrothermal alteration and the sedimentary environment by the study on many profiles in this area, with discovery of volcanic rocks for the first time in ore - bearing strata and ore bodies

    取的了如下主要果和認識: 1 、通過對礦區地層多條剖面的研究,對地層的層序、石類型、作用、熱液蝕及原沉積環境有了新的認識,特別是在賦礦地層及礦體中首次發現了
  8. The genesis of gold deposits is complex in this district, the type of quart - vein plus etch rock belongs to hydro thermally superimposed complex mineralization. the type of porphyry and scraping rock containing charcoal belongs to volcano sediment - alteration hydro thermally gold deposits, the formation of gold deposits is controlled by several factors

    本區金礦床的因比較復雜,石英脈+蝕型金礦屬于熱液疊加復合因礦床,含炭山碎屑型金礦屬於山沉積?熱液改造型層控金礦床。
  9. We deduce that it is a relic old crust that was brought upwards during the formation of neo - tethyan ophiolite. the step heating 40ar - ' 9ar spectra show that during 100ma, luobusha ophiolite suffered intensely alternation, which affected distinctly the k - ar system ; during 771ma some basalt formed in the country rock of xiubugabu ophiolite ; during 55ma, the pillow basalt of rikangba ophiolite affected by a strong thermal event ; all the variety of ages illustrates possible impacts of the subduction - collision between india and eurasia. through dissecting mainly the gabbro of luobusa ophiolite and studying the 40ar / 39ar

    ~ ( 40 ) ar ~ ( 39 ) ar階段升溫年齡圖譜顯示, 100ma左右羅布莎體經歷了較強的後期蝕作用,對其k ? ar體系造明顯影響; 77 1ma休古嘎布體圍中形玄武山集塊; 55ma日康巴石枕狀玄武受到較強熱事件影響;這些~ ( 40 ) ar - ~ ( 39 ) ar年齡上的化顯示了印度板塊與歐亞板塊俯沖?碰撞對該區的強烈影響。
  10. After the volcanic eruption of multi - phrase cycle - deformation, filling of basin, crustal uplifting event being studied, this dissertation tries constructing the different degree rhythm of magma activity corresponding with crust - mantle dynamic system, studying the crust - mantle deep processes. based on the studies on the characteristics of volcanic rhythm, igneous rocks assemblages, temporal and spatial distribution of igneous rocks, tectonic deformation, the author has util ized the methods of petrology, geochemistry, isotopic geology et al. to do research on the above - mentioned geological problems

    通過多次幕式山噴發-構造形-盆地充填-地殼隆升事件序列的釐定,從山活動節律特徵、構造組合類型、時空分佈及其演化和構造形的歷史記錄,利用石學、地球化學、同位素地學等方法,反演深部過程與淺部響應等來闡明造山過程,建立與不同級別漿活動節律對應的殼幔動力學系統,追索殼幔深部過程,已為當今地球動力學研究的前沿課題之一。
  11. The study of geological characteristics and geochemical conditions of mazhuangshan gold deposit shows that it is closely related with old metamorphic basement and volcano - magmatic activities as well as volcanics and volcaniclastics of mazhuangshan - mingshui superimposed volcanic basin, and controlled by structures derived from closure of late palaeozoic honghe basin

    摘要對馬莊山金礦地特徵及地球化學條件研究表明,馬莊山金礦的形與古老基底、漿活動及馬莊山一明水上疊盆地的山碎屑緊密相關,並受到晚古生代紅河盆地閉合而派生的構造控制。
  12. The average chargeability value of 798 sedimentary rock specimens is 2. 4 %, that of 1149 igneous rock specimens is 2. 99 %, and that of 436 metamorphic rock specimens is 3. 59 %, which implies that the metamorphic rock might be the source of metallic ore deposits

    數值統計結果顯示, 798件沈積的平均極化率為2 . 40 % , 1149件的極化率為2 . 99 % , 436件的極化率為3 . 59 % ,因此,是本區較好的金屬礦礦源。
  13. H " was calculated using the shannon - wiener formula : h " = ? pi ? pi e was calculated using the pielou ' s evenness index e : e = h ' hmax = h ' ? s the results showed that diversity index on different parent materials varied between 0. 49 to 1. 02, the different parent materials followed the sequence of igneous rock > sedimentary rock > metamorphic rock > unconsolidated material ; the evenness index on different parent materials varied between 0. 27 to 0. 64, the parent materials followed the sequence of igneous rock > sedimentary rock > metamorphic rock > unconsolidated material

    多樣性指數運用shannon指數公式計算,均勻度指數運用pielou指數公式計算。分析結果表明發育于不同母上的多樣性指數范圍為0 . 49 1 . 02之間,從高到低依次為、沉積和疏鬆物;土壤均勻度指數范圍為0 . 27 0 . 64之間,從高到低依次為、沉積、疏鬆物
  14. Based on the study on ree distribution characteristics of sinian low grade metamorphic rocks of the basement and cover volcanics, the author makes a discussion on the material source and the genesis of xiangshan volcanics, and suggests that xiangshan volcanics came mostly from the remelting of the upper crust, and the genesis should be attributed to the category of remelted granites

    摘要本文通過對相山山盆地基底震旦系淺、蓋層稀土元素分佈特徵的研究,探討相山的物來源及因,認為相山主要是上部地殼重熔的產物,其因應屬于重熔型花崗的?疇。
  15. It is very resembly representative island arc volcanic rock in the geochemistry character, so i demonstrate that a petrofabric formed tectonic activity section and island arc environment ; i also demonstrate that parametamorphite in the a petrofabric formed tectonic activity section. b petrofabric is very resembly a petrofabric in many aspects, so i think that b petrofabric also formed island arc environment, but volcanic activity obvious weakened in the b petrofabric stage. c petrofabric formed carbonatite mesa

    在地球化學特徵方面與典型島弧非常相似,得出a組形於構造活動區,形環境為島弧環境。 a組的副的原碎屑是快速堆積的,處于構造活動區。 b組和a組對應的石在各個方面都非常相似,所以形環境也為島弧環境,只是山活動在這期間明顯減弱。
  16. Hong kong experienced lots of land - making processes in its long geological history, hence various types of volcanic, igneous, sedimentary and metamorphic rocks could be found in the territory

    香港地歷史源遠流長,經歷過許多的造地過程,故境內可找到多種類的沉積
  17. Hydrocarbons commonly occur in sedimentary basins and are absent from intervening areas of igneous and metamorphic rocks

    在沉積盆地中,碳氫化合物很常見,而在間雜的中則找不到。
  18. Mainly thinking over ore - bearing rock series and giving consideration to ore - forming process, the author divides the gold deposits in fujian into four categories which include metamorphic rock category, volcanic rock category, sedimentary clastic rock category and igneous rock intrusive contact category

    採用以容礦系為主體兼顧礦環境和礦作用的分類原則,把福建省金礦劃分為型、型、沉積碎屑型和侵入內外接觸帶型四類。
  19. Selecting youxi - dehua - yongtai, zhenghe, taining and shanghang prospecting metallogenic provinces ( total area 2516 km2 ), which have good gold - finding prospective and relatively rich data, and using the method of characteristic analysis and information extraction to seek gold prospecting target, the author builds the gold deposit forecast models of metamorphic rock category and the volcanic rock category, determines 86 good gold - finding units in fujian and assesses the gold resource extent of the order v prospecting metallogenic provinces in shanghang, taining, zhenghe, and youxi - dehua - yongtai and jianyan, . which provides important reference basis for seeking gold deposits in next survey

    選擇尤溪?德化?永泰、政和、泰寧和上杭四處礦遠景較佳、資料水平較高的礦遠景區(總面積2516km ~ 2 ) ,利用特徵分析和信息量法進行找礦靶區優選,建立了型金礦和型金礦的預測模型,優選出有利礦單元86處。對上杭、泰寧、政和、德化?尤溪?永泰和建陽級礦遠景區的金資源量進行了估算,為省內下一步金礦的找礦工作提供了重要的參考依據。
  20. This paper particularly focuses on the theory and implementation of how to inverse underground structure by comparing incident wave and scattering wave, and recording the spare time of the waves, and forward calculations for igneous, metamorphic and sedimentary rocks are carried out to verify the feasibility

    著重論述了利用慢衰減電磁波的入射波和散射波的振幅關系,以及電磁波的走時關系反演地下介參數的基本原理及方法,同時,針對和沉積,通過正演理論計算,說明了慢衰減電磁波測深的可行性。
分享友人