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According to their mineral assemblages, the granulite xenoliths entrained by Cenozoic Hannuoba basalts are divided into four groups: felsic granulites, noritic granulites, two-pyroxene two-feldspar granulites and two-pyroxene granulites, with the two-pyroxene granulites most common.
根据矿物组合特征，汉诺坝玄武岩中的麻粒岩捕掳体可划分为四种类型：长英质麻粒岩、苏长质麻粒岩、二辉二长麻粒岩和二辉麻粒岩，其中以二辉麻粒岩最为常见。
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The deep-seated xenoliths entrained by the Cenozoic Hannuoba basalts can be divided into three groups according to their mineral assemblages:Ⅰ Granulites, including felsic granulites, noritic granulites, and dominantly, two-pyroxene granulites,Ⅱ Pyroxenites, including websterites, spinel pyroxenites, and garnet pyroxenites;Ⅲ Peridotites, including spinel lherzolites and spinelgarnet lherzolites.
根据新生代汉诺坝玄武岩中深源岩石捕掳体的矿物组合类型，将其分为主要的三大类：麻粒岩类中包括长英质麻粒岩、苏长质麻粒岩和二辉麻粒岩，辉石岩类包括二辉石岩、尖晶石辉石岩和石榴子石辉石岩，橄榄岩类则包括尖晶石二辉橄榄岩和尖晶石-石榴子石二辉橄榄岩。
- 更多网络解释与辉长苏长岩相关的网络解释 [注：此内容来源于网络，仅供参考]
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enstatite diopsidite：顽火透辉石岩
顽火苏长岩 enstatite norite | 顽火透辉石岩 enstatite diopsidite | 顽火透辉岩 marchite
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gabbro norite：辉长苏长岩
gabbro 辉长岩 | gabbro norite 辉长苏长岩 | gabbroid 辉长岩状
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gabbroid：辉长岩状
gabbro norite 辉长苏长岩 | gabbroid 辉长岩状 | gabbronite 硅铍钇矿
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gabbroid：辉长石状
辉长闪长玢岩类 gabbrodiorite porphyrite | 辉长石状 gabbroid | 辉长苏长岩 hydperite
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hypergenesis：表面蚀变
hypergene zone 浅成带 | hypergenesis 表面蚀变 | hyperite 辉长苏长岩
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hyperite：辉长苏长岩
hypergenesis 表面蚀变 | hyperite 辉长苏长岩 | hypermelanic rock 深暗色岩
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hyperite texture：辉长苏长结构
辉长苏长岩 hyperite | 辉长苏长结构 hyperite texture | 辉苏闪长岩 hyperite-diorite
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sanukite：玻苏安山岩
钠长苏安岩 santorinite | 玻苏安山岩 sanukite | 玻辉安山岩 sanukitoid