【摘 要】
：
在叶理状钾长-夕线石变泥岩中,纤维状夕线石常富集于由粗粒集合体构成的扁豆体之间的叶理中。这些集合体富含石英、长石、黑云母,有或无石榴石,堇青石和残留红柱石。大多数叶
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在叶理状钾长-夕线石变泥岩中,纤维状夕线石常富集于由粗粒集合体构成的扁豆体之间的叶理中。这些集合体富含石英、长石、黑云母,有或无石榴石,堇青石和残留红柱石。大多数叶理看来象细微褶皱翼。夕线石的聚集可能主要是由于纤维状夕线石集合体能够经受强烈的非同轴变形所造成的。这种变形表现为颗粒边界滑动(纤维滑动),并没有明显的位错聚集。而其他矿物在这些带中不稳定,所以富集于低应变的间叶理带。夕线石的产生,特别是叶理中夕线石的富集,得力于流体流动和局部碱性阳离子的淋滤,因此,强非同轴应变带中不稳定的矿物发生溶解并从这些带
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