鉛的同位素 的英文怎麼說
中文拼音 [qiāndetóngwèisù]
鉛的同位素
英文
actinium lead-
The test of sulfur and lead isotope of ores shows that mineralizing matter mainly comes from deep. the ore minerals are typical low - to - moderate - temperature hydrothermal minerals, such as stylotypite, galenite and chalcopyrite
對礦石中硫和鉛進行同位素測定,認為硫主要來自深部,顯示了地幔硫遭受少量地殼物質混入后的硫同位素組成。Through the study of characteristic of macroelement, microelement, rare - earth element, oxyhydrogen isotope, sulfur isotope, lead isotope, fluid inclusion etc, a conclusion can be drawn that metallogenic substance comes from the upper mantle with mixing of some substance from the upper crust latter. it is likely to have the same source with the surrounding rock
通過對礦床的常量元素、微量元素、稀土元素、流體包裹體特徵、氫氧同位素、硫同位素、鉛同位素等特徵的研究,認為成礦物質主要來源於上地幔,與周圍巖石存在著同源的可能性,後期有一定的上地殼物質混入,成礦作用有三期,分別與區內的花崗巖、二長花崗巖脈、雲煌巖脈有關。And preliminary studies indicate virtually uniform is topic composition of the lead from a single copper - ore source
而最初的研究表明,對于來自單獨一個銅礦石來源的鉛來說,其同位素構成幾乎是毫無二致的。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。On the basis of the composition analyses for 80 samples of bronze drums and some samples of ore, these tests detemine the lead isotopic of the samples, to obtain test data for deep research
摘要在對越南80個銅鼓樣品和相關銅器以及若干礦樣進行成份分析的基礎上,對樣品進行了鉛同位素測定,得出了一批可供進一步研究的實驗數據。A lead isotope ratio data base of ancient chinese bronzes
夏商周青銅器鉛同位素示蹤研究數據庫的構建It was also indicated by the studies on a large number of pb isotope that pb in ores of the deposit chiefly came from volcanic rocks in the strata and later intrusions with derivation of a little pb from the normal deposit stratum
大量pb同位素研究也表明,礦床的礦石鉛源跨越了下地殼、地幔和造山帶演化線,形成混合鉛帶,多集中於地幔和造山帶演化線附近,暗示pb主要來自地層中的火山巖和後期的侵入巖,少量來自正常沉積地層。Research on the mineral sources of bronze vessels in shang - zhou by lead - isotope ratio
從鉛同位素比值試析商周時期青銅器的礦料來源According to the comparison and analysis of mineral composition and geochemical characteristics of trace element, sulfur isotope, hydrogen and oxygen isotope, lead isotope and rare earth element in the gold ore and the altered spilite from the deposits of huachanggou gold mine, it was confirmed that the gold ore had obvious succession of the basic igneous rock
摘要通過對鏵廠溝金礦床金礦石和蝕變細碧巖礦物組成、微量元素、硫同位素、氫氧同位素、鉛同位素及稀土元素地球化學特徵地對比分析,得出金礦石對該基性火山巖存在明顯的繼承性。The plumbum of ores have some characteristics of the plumbum of earth ' s mantle and some characteristics of the plumbum of up per earth ' s crust
阿克提什坎金礦床不同地質體鉛同位素特徵表明,礦床鉛不是單一來源的正常鉛,而是混合型多來源的異常鉛。From the study of lead isotope, we know that the lava of erlangping is ocean lava - spilite keratophyre, it is the main origin of lead in time evolvement sequence and genesis
鉛同位素研究表明本區二郎坪群的火山巖為洋殼火山巖?細碧角斑巖,在時間演化序列上和成因上它們作為pb的主要源巖。Molding experiment on indicating meaning of lead isotopes in bronze
青銅器鉛同位素指示意義的范鑄實驗研究Abundant concentration of lead on the sample of bronze drum in viet nam and survey for lead isotopic
越南銅鼓樣品鉛的富集與鉛同位素測定Lead isotopic tracing and its future application in the mining environment assessment of liaoning province
鉛同位素示蹤技術及其在遼寧省礦業環境評價中的應用前景In 2002, wen et al. reported the contents of lead isotopes in 76 vietnamese timbals and 18 relative objects, but only single point measurement was made
摘要2002年韋冬萍等在對76面越南出土銅鼓及18件相關物件樣品進行鉛同位素測定時,用電子探針的方法進行了成份分析,但只作了單點測試。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。The isotopic composition of lead often varies from one source of common copper ore to another , with variations exceeding the measurement error ; and preliminary studies indicate virtually uniform is topic composition of the lead from a single copper - ore source
鉛的同位素構成經常在一種普通銅礦石來源與另一種銅礦石來源之間存在差異,其差異程度超出測量誤差;而最初的研究表明,對于來自單獨一個銅礦石來源的鉛來說,其同位素構成幾乎是毫無二致的。分享友人