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矾山岩体是一环状碱性超镁铁杂岩体。There is a kali-alkaline ultramafic complex in the Fanshan of Hebei.

黑云母一般是镁铁质及超镁铁质岩石中的次要成分。Biotite is a subordinate constituent of the mafic and ultramafic rocks generally.

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海山顶部的岩石是由蛇纹石化超镁铁质方辉橄榄岩组成。The rocks at the top of the seamount consist of serpentinized ultramafic harzburgite.

超镁铁质侵入杂岩体由纯橄岩，橄榄岩，辉石岩，辉长岩及它们的变质产物组成。The ultramafic intrusive complex is composed of dunite, peridotite, pyroxenite, gabbro and their metamorphic products.

近年来，应用地球动力学研究镁铁质-超镁铁质岩石演化取得了一些重要进展。Recently, several important progresses have been made in the geodynamics concerning the evolution of mafic and ultramafic rocks.

中国东部新生代玄武岩中丰富的超镁铁岩包体，是玄武岩浆喷出地表时取出的上地幔岩石标本。Cenozoic basalt in eastern China contains abundant ultramafic xenoliths which are specimens of pyrolites taken during basalt eruption.

矾山岩体为一偏碱性超镁铁岩-正长岩杂岩体，其中蕴藏着中国北方最大的岩浆型磷灰石矿床。Fanshan intrusive body is a complex body of meta-alkaline ultramafic rock-syenite. It hosts the biggest magmatic apatite deposit in north China.

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矾山岩体为偏碱性超镁铁岩正长岩杂岩体，其中蕴藏有我国北方最大的岩浆型磷灰石矿床。Fanshan intrusive body is made up of alkaline ultramafic rock-syenite in which there is the biggest magmatic apatite deposite in the north China.

稀土元素、微量元素组成与世界已知钾镁煌斑岩具有相同特征。Their REE and microelement 's composition exist the common characteristics with the world known lamproites. There are many ultramafic rock bodies.

陕西商南县松树沟橄榄岩体是秦岭造山带中具重要意义和争议较大的岩体。The Songsugou peridotite in Shangnan, Shaanxi Province is an important but petrogenetically debated ultramafic massif in the Qinling orogenic belt.

库地蛇绿岩套由下部超镁铁质岩、辉长岩、幔源型花岗岩和上部基性火山岩、复理石等成分构成，形成于震旦纪—寒武纪。Kudi ophiolite suite is composed of ultramafic rocks, gabbro, mantle source granitoid, basic volcanic rocks and flysch. It was formed during Sinian and Cambrian.

以窑沟橄榄辉石角闪石岩岩体为代表，研究了涞源岩基中超镁铁质岩石。This paper chooses the Yaogou hornblendite body, one of the two major ultramafic outcrops in the Laiyuan batholith, as a representative to carry out detailed research.

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松树沟超镁铁质岩体位于秦岭商丹断裂以北，是该地区出露最大的超基性岩体，以侵位方式与秦岭杂岩接触。The Songshugou ultramafic pluton north of the Shangdan fault is the largest ultramafic body in the East Qinling Orogen and assumes the emplacement contract with the Qinling complex.

本文对中国东部一些新生代玄武岩中二辉橄榄岩团块的结构进行了研究。The ultramafic nodules widely distributed in Cainozoic basalt in eastern China are regarded as fragments of upper mantle that were brought up to the ground surface by basaltic magma.

这些特征表明，浅色岩是幔源超基性岩浆晚期结晶分异的产物。All of these characteristics are in contrast with their host rock_serpentinite and show that the leucocratic rocks were produced by crystallization differentiation of ultramafic magma.

异剥钙榴岩的形成主要取决于超镁铁岩的蛇纹石化作用和钙交代程度，而与超镁铁岩的成因类型、构造属性和时代归属没有多大的关系。The formation of rodingites depends on the serpentinization and degree of calcic metasomatism, and has no relationship for genetical types, tectonic setting and age of ultramafic rocks.

蛇绿杂岩带由超镁铁质岩、辉长岩、玄武岩和少量硅质岩组成，形成于弧后扩张脊构造背景，成岩时代为寒武纪-奥陶纪。The ophiolite complex consists of ultramafic rocks, gabbro, pillow lavas and minor cherts, which formed in a tectonic setting of the back-arc spreading ridge during the Cambrian-Ordovician.