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属于角闪岩相产物。They belong to the amphibolite facies.

带内最高变质相达角闪岩相。The highest metamorphic facies in the zone reached amphibolite facies.

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榴辉岩转化成含帘石的斜长角闪岩。As a result, the eclogite was transformed to epidote-bearing amphibolite.

容矿围岩变质级别达到角闪岩相和麻粒岩相。The host rocks were metamorphosed to the amphibolite and granulite facies.

从大理岩→滑石矿体→斜长角闪岩具有明显的分带现象。It has obvious horizontal zoning from marble, talc ore body to amphibolite.

变质相多为角闪岩相，局部达麻粒岩相。Mostly metamorphic facies is amphibolite facies, partial up to granulite facies.

以大理岩为原岩的矿石品质优良，以斜长角闪岩为原岩的矿石品级较低。Grade of ore formed from marble is higher, that formed from amphibolite is lower.

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十字石的出现表明变质作用已达到低角闪岩相。The appearance of staurolite indicates that the metamorphism has reached the low amphibolite grade.

经过角闪岩相区域变质作用，形成了佛坪地区较为完整的孔兹岩系。The bedded me tamorphite series in Foping area had been formed by regional metamorphism of amphibolite facies.

在含柯石英榴辉岩中的石榴子石位错密度比角闪岩中的低。Microstructures of the garnet vary greatly from coesite-bearing eclogite to quartz eclogite and garnet amphibolite.

红宝石大理岩产于古老的动热变质带的变质杂岩中，变质强度为低角闪岩相。This ruby marble is occurred in an old metamorphic complex of dynamothermal metamorphism zone in-low amphibolite facies.

结果表明，宝音图群中斜长角闪岩原岩为岛弧环境中形成的玄武岩。The result suggests that the protolith of amphibolite in Baoyintu Group was basalt which formed in the island-arc environment.

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柴达木北缘鱼卡河地区的达肯大坂岩群可划分为斜长角闪岩岩组和片岩岩组。Dakendaba Group occurred in Iqe area, northern margin of Qaidam basin, can be divided into amphibolite assemblage and schist assemblage.

角闪岩包体来源于下地壳上部-中地壳下部位置，被上升岩浆带至地壳浅部。The amphibolite xenoliths were from the upper part of lower crust and the lower part of middle crust, bring up to the shallow area of crust.

变形由强烈的塑性变形到弱变形，变质由角闪岩相到低绿片岩相及低于低绿片岩相。The deformation was changing from plastic intensity to weakness and the metamorphic facies ranged from amphibolite to low-grade greenschist.

石榴角闪岩的原岩既可以是基性岩，如玄武岩或辉长岩，也可以是沉积岩如杂砂岩。The protoliths of the garnet amphibolite can be either basic magmatic rocks, such as basalt and gabbro, or sedimentary rocks, like greywacke.

在皖东嘉山南黄地区新元古代张八岭岩群之下，隐伏一套角闪岩相的TTG质片麻岩类。There is a suboutcrop of amphibolite facies TTG gneiss overlain by Neoproterozoic Zhangbaling Group at Nanhuang region in Jiashan, East Anhui.

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结果表明，该区的斜长角闪岩是由大洋拉斑玄武岩变质而成，变粒岩则是由酸性沉积岩变质而成。It was shown that the amphibolite was transformed from oceanic tholeiitic basalts and the leptynite was converted from acidic sedimentary rocks.

豫西秦岭群是东秦岭褶皱带的核心岩系，具角闪岩相变质并有不同程度的混合岩化。Being a member of the core complex in the Qinling folded belt the Qinling Group, is highly metamorphosed into amphibolite facies with migmatization.

东大山地区龙首山岩群形成于早元古代，是一套经角闪岩相变质改造的变质地质体。The Longshoushan Group of Paleoproterozoic age in the Dongdashan district is a metamorphic terrane composed of metamorphic rocks of amphibolite facies.