anorthoclase
- anorthoclase的基本解释
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歪长石, 钠斜微长石
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Structural water in anorthoclase megacrysts from alkalic basalts: FTIR and NMR study.
2000d。碱性玄武岩中长石巨晶的结构水：红外光谱和核磁共振谱研究。
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Pyroxene megacrysts formed under the temperatureof 1200.85-1288.85℃ and the pressure between 0.93 and 1.67GPa, amphibole megacrysts crystallizedunder the pressure of 0.83-0,89GPa, temperature about 1000℃, and anorthoclase maybe at thetemperature of 900℃ around.
辉石巨晶形成的温度压力范围分别为1200.85—1288.85℃和O.93—1.67Gpa，角闪石结晶温度在1000℃左右，压力为O.83一O.89GPa之间，歪长石巨晶结晶温度可能在900℃左右。
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A mass of pyrolite xenolith (such as peridotite andpyroxenide) and high-pressure mineral megacrysts (such as anorthoclase, augite and kaersutite)are found in cone sheets and BS volcanic rocks.
锥状岩席和BS火山岩包含有大量的上地幔岩石包体和高压矿物巨晶(歪长石、普通辉石和钛闪石)。
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anorthoclase：歪长石
钾长石是以不同比例的钠和钾互相取代,包括正长石(orthoclase)、微斜长石(microcline)和透长石(sanidine),及冰长石(adularia)和歪长石(anorthoclase),其在岩浆中结晶温度由高到低之顺序为透长石→ 正长石→ 微斜长石.
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anorthoclase：钠斜微长石
anorthite 钙长石 | anorthoclase 钠斜微长石 | anthracite 无烟煤
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anorthoclase：钠微斜长石(从矿)
anorthite 钙斜长石 | anorthoclase 钠微斜长石从矿 | antennaratio 天线比
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anorthoclase：钠微斜长石
退火 Anneal | 钠微斜长石 Anorthoclase | 颉颃作用 Antagonism
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anorthoclase basalt：歪长玄武岩
歪长石,钠微斜长石 anorthoclase | 歪长玄武岩 anorthoclase basalt | 长细晶花冈岩 anorthoclase-aplite granite
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