元素地球化學 的英文怎麼說
中文拼音 [yuánsùdeqiúhuàxué]
元素地球化學
英文
element geochemistry-
Through the ree charactheristics being studied, it suggests that the xenoliths from hannuoba, ximeng, and puning area have no the trend of lree enrichment, which ratios of lree / hree approximate 1. therefore, it is not different from archean lithospheric mantle
稀土元素地球化學研究表明，漢諾壩、錫盟、普寧等地區包體則無lree富集的趨勢， lree hree接近於1 ，因此它們與太古代巖石圈地幔不同，稀土元素特徵表明它們遭受了強烈虧損。Trace element geochemistry of cassiterite from the neves corvo massive sulfide deposit, portugal
塊狀硫化物礦床錫石的微量元素地球化學Further research of lithofacies pvove : lode country output points belongs to tidal - flat facies. and the two sides belong to littoral facies - estuarine facies. ore area petrochemistry analyse also prove : intraclast congeries silica rock in basin have higher cu, ag abundance than circumference pena. the prominence inhomogeneity of the cu distribution indicates reconstruct of the late construction
礦區內巖石化學測量也證明：盆地內發育的內碎屑堆積硅質巖比周圍巖石具有更高的cu 、 ag元素地球化學豐度值， cu元素分佈的顯著不均一性，表明了後期構造的改造作用。Based on an analysis of geochemical characteristics of rocks and trace elements as well as rare earth elements, this paper holds that they are products of crystallization differentiation of the same magma, that the major ore resource of this area is copper, and that gabbro - diabase is the main ore - bearing horizon
通過對巖石化學特徵和微量元素、稀土元素地球化學特徵的剖析，表明其是同一巖漿結晶分異的產物，本區主要礦產應為銅，輝長輝綠巖是主要的含礦層位。The elemental geochemistry features of the laowangzhai gold field, yunnan province
雲南老王寨金礦田元素地球化學特徵There are two sets of elements geochemical anomalies : one extends nw, and is controlled by regional faults ; the other extends ne, and intersects with the former taking on " v " form, and is important to mineral exploration. 3. almost all au deposits are situated in greenstone belt of tectonic sutures
元素地球化學場表現出兩個方向的特點：一組異常呈北西向展布，受區域構造控制；另一組異常呈北東向展布，與北西向異常交叉呈「 v 」字形，具有重要找礦意義。Elementary geochemical study on the roles of fluids during metamorphism
變質流體作用的元素地球化學研究Trace element geochemistry and plutonic process of peridotite and pyroxenite in the beishan, tarium area
輝石巖的微量元素地球化學特徵及其深部過程Detailed studies of the petrography, petrochemistry and geochemistry, indicate these volcanic rocks have high contents of aluminum and potassium and are intermediate to acid lavas and homoplasmic tufts
通過對該組火山巖的巖石學、巖石化學和元素地球化學研究，確認該火山巖為中性。The geochemistry of phosphorite of doushantuo formation in weng ' an, china : insights from trace elements and ree
貴州甕安磷礦陡山沱組地層元素地球化學特徵In this article, model of geological conception in panzhihua - xichang area is established, and then the authors used gis as the tool to analyze the pge ore - forming geological conditions, including geological structure, emeishan basalt, basic - ultrabasic rock and pge geochemical abnormal
本文在建立攀西地區鉑族元素礦床地質概念模型的基礎上，用地理信息系統（ gis ）分析了該地區的鉑族元素成礦地質條件，包括地質構造、峨眉山玄武巖、基性一超基性巖和鉑族元素地球化學異常特徵。The authors studied the characteristics of element geochemistry, mineral assemblage and microtexture of the white reticulate clay in the quaternary laterite of the dongting basin with some experimental analysis methods, such as chemical analysis, x - ray diffraction analysis, ir and sem analysis. the genesis of the vermiculate reticulate clay and the rhizomatic reticulate clay in the quaternary laterite of the dongting basin are discussed. the formation of crannies or holes in the soil and the transference of soil elements are absolutely necessary conditions to form the white reticulate clay in laterite
在野外考察的基礎上，運用化學全量分析x射線衍射分析紅外光譜分析和掃描電鏡微形貌分析等實驗方法和手段，對洞庭盆地第四系紅土地層中網紋的元素地球化學礦物組合特徵和微形貌特徵進行了系統研究，對洞庭盆地紅土地層中2種主要的網紋類型蠕蟲狀網紋和根狀網紋的成因進行了探討。The elemental geochemistry characteristics indicate that elements abundance is controlled seriously by grain size of sediment
元素地球化學特徵表明，元素的豐度受沉積物粒度控制明顯。Geochemistry of individual elements
個別元素地球化學The provenance of the sediment in middle okinawa trough during the last glacial maximum is the shelf of the east china sea. the characteristics of elemental geochemistry ascertain that the sediment was derived from the paleo - changjiang river
末次盛冰期沖繩海槽中部陸源物質來源於東海陸架，元素地球化學特徵顯示這些沉積物主要來源於古長江的入海物質。Comparison of the characteristic parameters of immobile elements, such as ree, sc, th, ti etc and of the characteristics of sedimentology and mineralogy comes to a conclusion that the provenance of the sediment is different in the last glacial maximum and in the sub - interglacial stage, and they have the traits of mixed source. during the last glacial maximum the sediment in the outshelf of the southern east china sea was affected weakly by changjiang river and they are probably derived from the coast mountains of zhejiang - fujian province, which are near the southern east china sea
通過對東海外陸架樣品的稀土元素和sc ， th ， ti等不活潑元素地球化學物源示蹤指標對比，再結合沉積學和礦物學特徵，判斷末次盛冰期與盛冰期以前的沉積物具有不同的物質來源，不同時期的沉積物都具有混合物源的性質，盛冰期東海南部外陸架沉積物受長江物源影響較小，可能來源於距東海南部較近的浙閩沿海山地。Elemental geochemical records of modern seafloor hydrothermal activities in sediments from the central okinawa trough
沖繩海槽中部現代海底熱液活動在沉積物中的元素地球化學記錄The study covers regional geology, the physicochemical conditions of cu - ag polymetallic mineralization area, transport forms of copper and silver, the ore - forming geochemical mechanism of cu & ag, the geochemical characters of major element, trace element and lanthanon in mineralization field, the ore - forming age and geochemical mode, and so on
研究內容包括：區域地質和礦田地質，銅銀多金屬礦形成的物理化學條件，銅銀遷移形式，銅銀富集的地球化學機理，礦田常量元素、微量元素和稀土元素地球化學特徵，白秧坪銅銀多金屬礦田成礦時代和地球化學模式等。Ree geochemistry of doushantuo phosphorites and paleoenvironmental changes in weng ' an area, south china
貴州甕安陡山沱組磷塊巖的稀土元素地球化學特徵與沉積古環境Rees geochemistry of doushantuo phosphorites and modification during post sedimentary stages in weng ' an area, south china
貴州甕安陡山沱組磷塊巖稀土元素地球化學特徵與沉積期后變化分享友人