Four different lithofacies are recognized as peridotite+pyroxenite, norite+gabbronorite, gabbro+diabase, and diorite including ultramafic rocks to intermediate rocks from core to margin of the intrusive body.3.
2.杂岩体可分为四个岩相带(橄榄岩+辉石岩相,苏长岩+辉长苏长岩相,辉长岩+辉绿岩相,闪长岩相),包括中性-基性-超基性的多种类型岩石组合而成。 显微镜岩相学研究查明,四方台杂岩体岩石比较新鲜,基本无变质和蚀变。
参考来源 - 四方台镁铁—超镁铁质杂岩体的地球化学特征及其大地构造意义·2,447,543篇论文数据,部分数据来源于NoteExpress
以上来源于: WordNet
N an altered dolerite 辉绿岩 [英国英语]
What are the characteristics of diabase?
辉绿岩的特征是什么?
The main rocks in the complex are gabbro, gabbro-diabase, pyroxenite and olivine-pyroxenite etc.
杂岩体主要岩石类型为:辉长岩、辉长辉绿岩、辉石岩、橄榄辉石岩等。
The diabase and lamprophyre are typical mantle source rock while the granite pegmatite is typical crustal source rock.
其中辉绿岩和煌斑岩是典型的幔源岩,花岗伟晶岩则是典型的壳源岩。
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