carbonate minerals的意思

carbonate minerals中文翻譯：

[礦物]碳酸鹽礦物

相似詞語短語

minerals───n.礦物；礦產，礦產品（mineral的復數）；礦物質

carbonate───v.溶解碳酸鹽；轉成碳酸鹽；n.碳酸鹽

bijoux minerals───礦物首飾

spirifer minerals───螺旋體礦物

fugacious minerals───閃石

bare minerals───裸礦

dipropyl carbonate───[化] 碳酸二丙酯

strontium carbonate───[無化]碳酸鍶

carbonate rock───[巖]碳酸鹽巖

雙語使用場景

Heavy calcium carbonate coarse whiting, which is made of natural calcium carbonate minerals such as calcite, marble grinding.───重質碳酸鈣簡稱重鈣是由天然碳酸鈣礦物如方解石、大理石磨碎而成。

that carbonate minerals are aragonite, high-Mg calcite, and lesser dolomite, ankerite and siderite.───碳酸鹽巖中自生碳酸鹽礦物主要為文石、高鎂方解石，少量白云石、鐵白云石和菱鐵礦。

Made of limestone, tufa forms as a byproduct of the precipitation of carbonate minerals from surrounding water.───灰巖是由石灰巖所組成，它是在其周圍湖水里的碳酸鹽礦物沉淀的副產品。

Made of limestone, tufa forms as a byproduct of the precipitation of carbonate minerals from surrounding water.───凝灰巖是由石灰巖所組成，它是在其周圍湖水里的碳酸鹽礦物沉淀的副產品。

Evaluation of Oxygen Stable-isotope Fractionation among Different Carbonate Minerals in the Sediments of Lake Qinghai───青海湖沉積碳酸鹽礦物之間氧同位素分餾的評估及其環境意義

Study on Visible Photoluminescence and Absorption Spectra of Rare- earth Fluoro- carbonate Minerals───稀土氟碳酸鹽礦物的光致發光譜和吸收譜研究

Inversion and Recrystallization of Carbonate Minerals───碳酸鹽礦物的轉化作用和重結晶作用

C-O and Sr-Nd isotopic geochemistry of carbonate minerals from gold deposits in East Shandong, China───膠東金礦床碳酸鹽礦物的碳-氧和鍶-釹同位素地球化學研究

Stacking faults and intergrowth in crystal structure of alkaline-cerium fluorine carbonate minerals───鹼土-鈰氟碳酸鹽礦物晶體結構中的無序堆垛和交生

英語使用場景

Diagenetic minerals are mainly thin film shaped chlorite and increasing shaped quartz minerals. There are autogenous apatites, filled silicious and carbonate minerals as well.

X-ray studies show that carbonate minerals are aragonite, high-Mg calcite, and lesser dolomite, ankerite and siderite.

Fluor carbonate minerals from the late stage veins have relatively low carbon and oxygen isotopic values, implying an involvement of mantle derived solution.

Made of limestone, tufa forms as a byproduct of the precipitation of carbonate minerals from surrounding water.

This method produces the following colour differentiation in carbonate minerals: Calcite Varying through very pale pink to red.