長英粒變巖 的英文怎麼說
中文拼音 [zhǎngyīnglìbiànyán]
長英粒變巖
英文
leptite-
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,研究區長石砂巖物源母巖包括變質巖、沉積巖與火成巖,但從發育大量棕色石英顆粒來看,物源以變質巖為主。The cathodoluminescence ( cl ) analysis shows the quartz reflects an abundance of brown color, blue - purple, dark blue, dull color, and no cl color for quartz overgrowth, while feldspar shows light blue, yellow - green, yellow - brown, green and brown cl colors. the calcite reflects bright orange - yellow for non - ferroan calcite and dull orange - brown cl colors for ferroan calcite
陰極發光分析證實,砂巖中石英顆粒陰極發光顏色較深,主要位棕色、藍紫色、深藍色,石英加大變不發光;長石顆粒陰極發光顏色主要位淺藍色、黃綠色、綠色、棕黃色等;無鐵方解石陰極發光顏色為鮮艷桔黃色,鐵方解石陰極發光顏色為暗桔黃色。
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