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斜长石

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Plagioclase is a continuous solid solution series of albite anorthite, but its crystal structure is in continuous, which can be divided into several feldspar areas with different structure and attachment .

斜长石是钠长石-钙长石的连续固溶体系列,但在晶体结构上并不连续,可以划分成几种结构和连生不同的长石区。

Plagioclase is usually white-colored with perfect cleavage and albite twin s.

斜长石通常呈白色,具有完全解理和聚片双晶。

Plagioclase is usually white-colored with perfect cleavage and albite twins.

斜长石通常呈白色,具有完全解理和聚片双晶。

The mineral assemblage of mafic-intermediate lavas mainly contains pyroxene and plagioclase, and rarely with amphibole and bitotite.

中基性熔岩的主要造岩矿物是斜长石和辉石,几乎没有角闪石和黑云母。

Dark colored, fine-grained, and composed primarily of the feldspar mineral Calcic Plagioclase and the amphibole mineral Pyroxene.

深色,细粒度,主要组成为长石矿物类的钙斜长石和闪石矿物类的辉石。

Using conventional garnetbiotitemuscoviteplagioclasequartz geothermobarometry, pT conditions were estimated to be 590610 ℃ and 0.951.14 GPa for the Huilongsi Formation, and 630650 ℃ and 0.650.89 GPa for the Zuolaozhuang Formation, in agreement with lower and upper amphibolite facies, respectively.

运用传统的石榴石黑云母白云母斜长石石英地质温压计估算回龙寺组的变质pT区间为590~610 ℃、095~114 GPa,左老庄组为630~650 ℃、065~089 GPa,分别相当于低角闪岩相和高角闪岩相。

Kb, probably in the crust-mantle transition zone. The plagioclase phenocrysts are dominantly andesine with reverse zoning, and those of hornblende are Al-rich (Al2O3 ~15.9 wt%), indicative of high-pressure crystallization.

斜长石斑晶主要为中长石且具反向分带,而富铝的角闪石斑晶(Al2O3 ~15.9 wt%)也反映了高压结晶的特点。

The anorthite component of plagioclase from Kela 2 reservoir was dissolved so completely by the pore fluid that the dissolution made great contribution to the pore volume, and the albite component suffered partially dissolution; by contrast K-feldspar did not dissolved in the ground water at all.

克拉2 气田中斜长石骨架颗粒中的钙长石组分基本上遭受了彻底的溶蚀,对次生孔隙的贡献较大,钠长石溶蚀程度有限,而钾长石基本上不被溶蚀。

In high strain domains, due to the decomposition of biotite and plagioclase, fibrous sillimanites were concentrated while in the low strain places the microscopic fibrous euhedral sillimanites were developed between plagioclase and quarts grains.

在高应变域,黑云母和斜长石分解,纤维状矽线石富集,低应变域则可有少量不定向显微纤状自形矽线石发育于斜长石和石英粒隙之间,因此这些矽线石不能反映高温条件。

The XRD and SEM/EDX analyses demonstrated that minerals in Beijing PM10 were clay and quartz, plagioclase, potassium feldspar, albite, calcite, dolomite, hematite, pyrite, magnesite, gypsum, and laumontite, in descending order.

XRD及 FESEM/EDX单颗粒分析表明,北京市PM10中的矿物颗粒以粘土矿物和石英为主,另外还有斜长石、钾长石、钠长石、方解石、白云石、赤铁矿、黄铁矿,菱镁矿、石膏、浊沸石等,矿物颗粒表面的硫化现象常见。2002特大沙尘暴颗粒物中的矿物的含量自大到小分别为粘土矿物、石英、斜长石、方解石、钾长石、赤铁矿、黄铁矿、角闪石和石膏。

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