1、

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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2、

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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3、

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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4、

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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5、

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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6、

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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7、

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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8、

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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9、

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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10、

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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