carbonate minerals 中文意思是什麼
carbonate minerals
解釋
碳酸鹽礦物-
Carbonation is the combination of carbonate or bicarbonate ions with minerals.
碳酸作用是碳酸根離子或重碳酸根離子與礦物的化合作用。 -
Minerals in deposit are made up simpler, the metal minerals are pyrite, chalcopyrite in second, and littler natural gold ; the veinstone minerals are quant, feldspar and carbonate
礦床礦石礦物組成較簡單，金屬礦物以黃鐵礦為主，其次為黃銅礦，有一定量的自然金；脈石礦物以石英、長石、鐵碳酸鹽為主。 -
The main control factors of carbonate of preservation for information of seawater are : a ) the components of original minerals ; b ) the primary porosity of rock ; c ) the content of terrigenous elastics of carbonate rocks
有如下3個主要控制因素： a ）原始礦物組成； b ）巖石的原生孔隙度； c ）碳酸鹽巖中陸源碎屑礦物的含量。 -
The characteristic frequencies of the raman and infrared spectra of the fergusonite and aeschynite group minerals, monazites and the rare earth fluoro - carbonate minerals have been determined and assigned
（ 3 ）變生態礦物拉曼光譜的強度很弱、譜線寬而彌散，而退火晶態礦物的拉曼譜峰強而尖銳。 -
With the intermittent activity of hot fluid containing cc ^, ferrous carbonate minerals dissolved and precipitate repeatedly many times. in addition, dissolution of shells and feldspars, decrease of chlorite and increase of kaolinite could be found
隨著富co _ 2熱流體多次間歇性入侵導致了含鐵碳酸鹽礦物的反復多次溶解和沉澱、生物介殼大量溶蝕和長石鑄模孔的形成以及綠泥石消失、高嶺石增加等。 -
Other non metallic minerals and superfine powder such as ground quartz, magcogel, kaolin powder, light calcium carbonate, dolomite powder, barium sulfate and so on
如石英粉、膨潤土粉、高嶺土粉、輕質碳酸鈣、白雲粉、硫酸鋇等非礦粉體。 -
The products scope of chuanshi minerals processing factory : mica, vermiculite, quartz sand, colored grit, cobble, tourmaline, light calcium carbonate, feldspar, feldspar powder, marble, etc
靈壽縣川石礦產加工廠生? ?品范圍： -
The dynamics study of carbonate - clay minerals reactions shows that high temperature will benefit the reactions process and high pressure will be disadvantageous to the reactions
根據co _ 2生成反應的熱力學計算，溫度的增加有利於碳酸鹽礦物與粘土礦物作用形成co _ 2 。 -
In order to evaluate resource objectively, it is very important to find out the origin and the main source of co2 and to study the distribution pattern of hydrocarbon, nonhydrocarbon gas and probe the controlling factors, diagenetic evolution of different reservoirs ( rich in co2 or rich in cflo and the relation between diagenetic features and co2 have been studied systematically by using conventional and advanced techniques and the integrated the methods of petrology and geochemistry. based on the petrologic and geochemical data as well as dynamics reactions of carbonate ? lay minerals, the origin and distribution of co2 have been synthetically discussed
論文中應用常規及先進的測試技術，採用巖石學與地球化學相結合的方法，重點研究本區淺層氣藏富co _ 2儲層與富ch _ 4儲層的成巖演化特徵及其與co _ 2的相互關系，並通過天然氣的地球化學研究以及碳酸鹽礦物與粘土礦物反應形成co _ 2的熱力學分析，對co _ 2來源及分佈進行了初步分析和探討。 -
Among the discrimination criterion controlling the alteration of carbonate, neither cathodoluminescence of the carbonate minerals nor t he content of sr can act solely as discrimination criterion for controlling the alteration of marine carbonate
在碳酸鹽的陰極發光性、 sr含量和mn sr比值三個判斷成巖蝕變性的標準中，陰極發光性和sr含量不能單獨作為判斷標準來檢測海相碳酸鹽礦物的成巖蝕變性。 -
On the contrary, the reservoirs that were not influenced by hot fluid just were in early diagenetic stage b. 2. based on the synthetic analysis of varied data, the mechanism of repeated dissolution and precipitation of ferrous carbonate minerals has been discussed
在進行充分的巖石學研究基礎上，利用電子探針、穩定同位素及包裹體分析數據，探討了異常成巖演化儲層中含鐵碳酸鹽礦物反復溶解和沉澱的機理。 -
When diapir fractures opened, entering of hot fluid into reservoirs may cause dissolution of carbonate minerals, and when diapir fractures closed, carbonate minerals precipitated in high temperature condition
底辟斷裂開啟時，深部富c02熱流體進入儲層，導致碳酸鹽礦物溶解；通道閉合時，高溫使碳酸鹽礦物沉澱。
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