在榴辉岩带中存在大量的石榴角闪岩(退变榴辉岩)，其在产状、岩性及矿物组合方面与榴辉岩非常相似。
In every eclogite zone there are abundant garnet amphibolites which look very like eclogites both in occurrence and minerals assemblage.
在榴辉岩带中存在大量的石榴角闪岩(退变榴辉岩)，其在产状、岩性及矿物组合方面与榴辉岩非常相似。
In every eclogite zone there are abundant garnet amphibolites which look very like eclogites both in occurrence and minerals assemblage.
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