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变粒岩地块的构造走向是弧形。The tectonic trends in the granulite massif are arcuate.

麻粒岩体呈无根的透镜状。The granulite bodies have no roots and occur mainly as lenses.

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攀西麻粒岩是扬子陆块西缘康定杂岩的重要代表。The Panxi granulite is the most important part of Kangding complex.

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.

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.

麻石旋风床式除尘装置属于一种除尘器。The utility model relates to a granulite cyclone bed deduster, belonging to a deduster.

矿层赋存于早元古界辽河群里尔峪组含硼变粒岩段。The ore bed hosts in boracic granulite of Lieryu formation, Liaohe group of lower proterozoic.

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太古宙麻粒岩带就是太古亩地壳发生刚性板块运动的直接产物。Archaean granulite belts are just the product of plate-tectonic movement of rigid Archaean crust.

河北省宣化地区的高压麻粒岩带是非常具有研究意义的。The high pressured granulite belts in the Xuanhua area of Hebei Province are very worthy of being studied.

此外，对除尘器的结构形式，安装施工质量，麻石的选用等也进行了一些探讨。Also, some work has been conducted on scrubber structure and installation, and granulite selection as well.

内蒙古大青山太古宙麻粒岩带的变质构造演化及金的成矿②。Metamorphic and Tectonic Evolution of the Archean Granulite Belt of MT. Daqingshan and Gold Mineralization, Inner Mongolia, Chi II.

威海—乳山麻粒岩带是苏北—胶南构造混杂岩带北东段的北西边缘带。The Weihai Rushan granulite belt is the northwestern marginal zone of the northeastern section of the Subei Jiaonan tectonic melange zone.

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在东南极普里兹湾拉斯曼丘陵地区变泥质岩和长英质片麻岩中，定向分布着透镜状、扁豆状和香肠状镁铁质、超镁铁质麻粒岩。Oriented distributed mafic granulite lenses, pods and boudins occur in metapelitic and leucogneiss in the Larsemann Hills, Prydz Bay, East Antarctica.

从岩石组合来看，主要为混合岩、黑云母斜长片麻岩、斜长角闪岩，变粒岩类及少量残留麻粒岩组成。From the rock composition, it is mainly migmatite, biotite plagioclase gneiss, amphibolite, and a small amount of granulite which is composed of residues.

在内蒙古东部喀喇沁地区早中生代大营子闪长岩中首次发现基性麻粒岩捕虏体。The mafic granulite xenolith was first reported to have occurred in Early Mesozoic diorite in Harkin region, Eastern Inner Mongolia Autonomous Region, China.

在苏鲁超高压变质带荣成蓝晶石榴辉岩中，发现一具有特殊结构和地球化学特征的石榴辉石岩。Eclogite facies garnet pyroxenolite xenoliths in Hannuoba area show the typical layered cumulate structures and crystalloblastic textures of granulite facies.

通过麻粒岩地体以及火山岩中麻粒岩捕掳体的研究，使人们对地球深部的物质组成和结构有了直接的了解。By research of granulite terranes and granulite xenoliths in volcanic rocks, composing and structure of deep substance in the earth could be realized directly.

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东南极拉斯曼丘陵出露的麻粒岩相泥质片麻岩和镁铁质麻粒岩经历了复杂的变形变质历史。Granulite facies pelitic gneiss and mafic granulite outcropping in the Larsemann Hills, East Antarctica, underwent a complicated deformational metamorphic history.

元古代基底岩石中的云母片岩、片麻岩、花岗片麻岩、基性麻粒岩被压扁拉长且强烈糜棱岩化。Flattened-elongated-type mica-schist, gneiss, orthogneiss and basic granulite blocks of Proterozoic basement are involved in this zone, which are strongly mylonitized.

晋冀蒙三省交界的怀安-大同一带基性麻粒岩有保存完好的变质反应结构。Huaian Datong region on the bounder of Hebei Shanxi Inner Mongolia is one of the most important area where the Archean granulite complex is relatively completed exposed.