granulite

Archaean granulite and subdivision of lower crust in eastern hebei, China

冀东太古宙麻粒岩及下地壳分层的讨论

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Archaean era granulite facies metamorphite series are extensively outcropped in Sa-heqiao, Hebei province.

冀东迁西洒河桥是太古代麻粒岩相变质岩系广泛出露的地区.

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The amphibolite and basic granulite may be comparable to the world's metamorphic tholeiite.

斜长角闪岩和基性麻粒岩可与世界变质拉斑玄武岩对比.

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Garnet pyroxenite occurs as lenses in granulite-facies metamorphic granitic gneiss and pelitic schist in the Namjagbarwa Group-complex of the eastern Himalayan tectonic syntaxis.

在东喜马拉雅构造结南迦巴瓦岩群中，石榴辉石岩呈透镜状产于麻粒岩相变质的长英质片麻岩和泥质片岩之中。

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A TEM Study of Deformed Quartz and Garnet in the Mafic Granulite from the Southern Tianshan, China

南天山基性麻粒岩中变形石英和石榴子石的TEM研究

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The granulite facie rock shows lenticulars, mainly outcrops at about 500 meters to the town, east of river. The major minerals of these rocks are diopside, plagioclase, hornblende, biotite and garnet.

其中麻粒岩主要出露于佛坪县城南约500m河东岸，呈条带状和透镜状产出，其矿物组成以透辉石、斜长石、角闪石、黑云母及石榴子石为主。

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A dark, fine-grained igneous rock; diabase. The amphibolite and basic granulite may be comparable to the world's metamorphic tholeiite.

粗玄岩，辉绿岩一种暗色微粒火成岩；辉绿岩斜长角闪岩和基性麻粒岩可与世界变质拉斑玄武岩对比。

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The ore bed hosts in boracic granulite of Lieryu formation, Liaohe group of lower proterozoic.

矿层赋存于早元古界辽河群里尔峪组含硼变粒岩段。

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the metamorphic characteristics of granulite facies rocks in the laixi-pingdu area in eastern shandong province

胶东莱西&平度一带麻粒岩相岩石的变质作用特征

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Veiws evidently intercalate into biotite granulite of the Boluotai Formation of the Zhuzhangzi Group.

花岗斑岩主要由钾长石、石英、更长石及黑云母组成.

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Shushui rock group remains in Xiyao gneiss, and made up of amphibolite, magnetite quartzite, biotite granulite, calc-schist and dolomitic marble.

涑水岩群残存于西姚片麻岩之中，是由斜长角闪岩、磁铁石英岩、黑云变粒岩、钙质片岩和白云质大理岩组成。

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Metamorphic PTT path of the Archean granulite-facies terrane in Jining district, Nei mongol, and its tectonic significance

内蒙集宁地区太古宙麻粒岩相变质作用的PTt轨迹及其大地构造意义

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The Lower Continental Crust Composition Based on Discriminant Analysis of Global Granulite Terranes

全球麻粒岩相地体与大陆下地壳成分模型

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Mineralogical Characteristics of Cordierites in Krn Hy Crd Granulites from the Larsemann Hills, East Antarctica THE CORDIERITE-SILLIMANITE ASSEMBLAGE IN THE ARCHAEAN GRANULITE BELT ON NORTH CHINA PLATFORM AS AN INDICATOR FOR LOWPRESSURE GRANULITE FACIES

东南极拉斯曼丘陵柱晶紫苏堇青麻粒岩中堇青石的矿物学特征华北地台太古代麻粒岩相带的堇青石-夕线石组合：低压麻粒岩相的标志

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Tectonic patterns in granulite terranes were dependent upon superposition of different deformation series.

麻粒岩区的构造样式取决于以上构造变形序列的相对影响程度。

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a present study and comment on granulite facies terrene

麻粒岩相区地质研究现状及评述

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The granulite facies were resulted from the regional high-temperature metamorphism with medium pressure. The metamorphism evolution was the retrogressive metamorphism with approximate isobaric cooling ( IBC) and counter clockwise PTt path.

麻粒岩相是中压区域高温变质作用的产物，变质作用的演化为退变质、近等压冷却（IBC）反时针型的PTt轨迹。

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These data suggest that the granulite facies metamorphism lasted for about 27 Ma and was related to crustal thickening associated with the Early Paleozoic continental collision between the Qilian and Qaidam blocks, and to subsequent thermal relaxation and exhumation.

这些年龄结果显示麻粒岩相变质作用持续了大约27Ma，这可能与早古生代祁连地块与柴达木地块碰撞作用所引起的地壳加厚和后来的热松驰有关。

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The Archaean rocks widely exposed in the area studied belong to the Qian-xi Group of granulite facies, including granulite, charnockite, pyroxene ( and/ or amphibole)-plagioclase gneiss, amphibolite and so on.

研究区内广泛出露的太古代岩石属于迁西群麻粒岩，包括麻粒岩、紫苏花岗岩、辉石-斜长片麻岩、角闪岩等。

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The granulite facies retrograded stage with calcite+ dolomite+ diopside+ ilmenite+ phlogopite+ spinel ± orthopyroxene;

麻粒岩相退变质阶段，矿物组合主要为方解石+白云石+金云母+镁橄榄石+透辉石+钛铁矿+尖晶石±斜方辉石等；

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Granulite facies ultrahigh temperature metamorphism ( G-UHTM) is documented in the rock record predominantly from Neoarchean to Cambrian;

麻粒岩相超高温变质作用（G-UHTM）主要发育于新太古代至寒武纪岩石中；

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The Weihai Rushan granulite belt is the northwestern marginal zone of the northeastern section of the Subei Jiaonan tectonic melange zone.

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。

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The upper crust is mainly composed of slates, phyllites, schists, granulite of greenschist facies ( partly low-amphibolite facies) and granite intrusions, and sedimentary rocks at the top.

上地壳主要为绿片岩相（部分低角闪岩相）的板岩、千枚岩、片岩、变粒岩以及花岗岩组成，顶部为沉积盖层。

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