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1·Felsic gneiss is the most widely distributed rock type in Archean metamorphic complex areas.

长英质片麻岩是太古宙变质杂岩区最主要的岩石类型。

2·The metamorphic complex in study area can be divided into ji an rock group and Laoling rock group.

通化地区早元古代变质杂岩可划分为集安岩群和老岭岩群。

3·The metamorphic complex has a stripping fault (dynamic decollement belt of metamorphic deformation) contact with over Devonian strata.

其与上覆盖层—泥盆纪地层为剥离断层（动力滑脱变质变形带）接触。

4·It has many similarities to the greenstone belt in respect to the sequence of metamorphic complex, petrochemistry and trace element characters.

从变质杂岩地层层序、岩石化学、微量元素特征来看，它与绿岩带有许多相似之处。

5·In the area of Zhoukoudian, Beijing, there is a metamorphic complex compo-sed of gneiss, amphibolite migmatites and mylonites, along with the Fangshan intrusive body.

北京周口店地区房山岩体周围，分布有一套由片麻岩、斜长角闪岩、混合岩、糜棱岩等组成的变质杂岩。

6·According to the metamorphic rock assemblages and their characteristics, Whole Archean metamorphic rocks can be subdivided into Jianping Complex and Dayingzi Croup.

按岩石组合和特征，整个变质岩系被划分为建平变质杂岩和大营子群。

7·The pre Sinian metamorphic series in the Micang Mountain area on the northern margin of the Yangtze Craton consist of the Houhe Group Complex, the Bajiaoshu Gneiss Complex and the Huodiya Group.

扬子克拉通北缘米仓山地区前震旦纪变质岩系由后河岩群、八角树片麻杂岩和火地垭群组成。

8·The ultramafic intrusive complex is composed of dunite, peridotite, pyroxenite, gabbro and their metamorphic products.

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。

9·The supracrustal sequences in the dabie complex in northeastern hubei belongs to a late archean stratified metamorphic sequences.

鄂东北大别杂岩中的表壳岩系属于晚太古代层状变质岩系。

10·The Karamaili ophiolite complex in East Junggar of Xinjiang province was composed of metamorphic peridotite, gabbro, diabase and basic lava.

新疆东准噶尔卡拉麦里蛇绿混杂岩的岩石组合为变质橄榄岩、辉长岩、辉绿岩和基性熔岩等。