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The Na-rich zeolites from Boron, California

机译:来自加利福尼亚州硼的富含富含沸石

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Unusually Na-rich zeolites have been found in cavities in blocks of basalt on the waste dump at the US Borax Mine at Boron, 135 km northeast of Los Angeles, California. The basalt underlies Miocene basin fill deposits, consisting of sand, shale, tuff, and Na-borate deposits. The zeolites show two generations of growth. Early gmelinite-Na is overgrown by later chabazite-Na, and early clinoptilolite-Na is overgrown by heulandite-Na. Other zeolites in these cavities are phillipsite-Na, analcime, Na-rich mordenite, and mazzite-Na. The occurrence of searlesite and borax, attests to the saturation of the basalt with a sodium borate solution at least at some stage. The extreme Na-rich compositions of all the zeolites strongly indicate cation exchange in Na-borate brine, while the overgrowth crystals may have grown in the brine.
机译:在加利福尼亚州洛杉矶东北135公里的美国Borax矿的废物倾倒的玄武岩中的玄武岩块中发现了异常的沸石。玄武岩下潜盆地填充沉积物,由砂,页岩,凝灰岩和Na-硼酸盐沉积物组成。沸石显示出两代生长。早期的转化基因 - Na覆盖过来的Chabazite-Na,并且早期的临床暴露于海尔(Heulandite-Na)覆盖。这些腔体中的其他沸石是紫百分点-Na,analcime,富含富含菱形和麦芽石。 Searlesite和Borax的发生,至少在某个阶段至少证明玄武岩的饱和硼酸钠溶液。所有沸石的富含Na的富含Na的组合物强烈表示在硼酸盐盐水中的阳离子交换,而过度生长晶体可能已在盐水中生长。

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