The calc-alkaline suite is typical of those emplaced in subduction-zone environments, whereas the hyperalkaline suite is associated with major deep crustal faults.
钙碱性岩套是侵位于俯冲带的典型岩套，而碱性岩套则与较大的地壳深断裂有关。
The calc-alkaline suite is typical of those emplaced in subduction-zone environments, whereas the hyperalkaline suite is associated with major deep crustal faults.
钙碱性岩套是侵位于俯冲带的典型岩套，而碱性岩套则与较大的地壳深断裂有关。
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