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There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.

构造破碎带具有明显对称分带性:破碎带中心为体,向两侧依次为榍透辉长英岩带、云母长岩带,并逐渐过渡为围岩。因类型为沿构造破碎带产出热液交代脉型。

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In the slag both the titanaugite and Ti-rich diopside almost vanish and most of the dispersed Ti component has been transferred into perovskite phase and then fully grows and coarsens.

赋存状态也发生相应改变,渣中攀钛透辉和富钛透辉几乎消失,渣中弥散分布钛组分大部分转移到钙钛相,而且实现长大和粗化。

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also-ran, alsorunner, Alstom, Alston, alstonamine, Alstonia, alstonia-leaf, alstonin, alstonine, alstroemeria,

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3G, 401(K), a,

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