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变质岩

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The pre-Jinning cycle belongs to the stage of geosyncline development.

前晋宁旋回和晋宁旋回属地槽发展阶段,由变质岩系组成地台的褶皱基底。

In the Appalacians, on the other hand, you can find metamorphic rocks approximating as gneiss and schist.

在Appalacians ,另一方面,你可以找到变质岩逼近作为片麻岩和片岩。

Gneiss, a metamorphic rock, can be commonly found in Precambrian areas.

片麻岩,变质岩,可以发现,在常见的前寒武纪地区。

Located in Songxian Henan province, the Leimengou Mo-mineralized granite porphyry is a small stock with an exposed area of 0.77 km~2, which emplaced in the metamorphic rocks of Taihua Group.

雷门沟钼矿化花岗斑岩体位于河南省嵩县境内,呈一小岩株状侵位于太华群变质岩系中,出露面积约0.77km~2,在其接触带具有爆发角砾岩。

Geological and geochemical features suggest that the bimodal volcanism took place in rift setting of continental margin, basic magma originated from not strongly depleted mantle, and rhyolite derived from the original melt formed by partial melting of granulite facies orthometamorphite in lower crust.

地质和地球化学特征指出吕梁群上部的双峰式火山岩形成于大陆边缘的裂谷环境,其中的玄武质岩浆起源于亏损程度较低的上地幔,并受到了陆壳物质的混染。酸性端元是由下地壳麻粒岩相正变质岩的部分熔融形成。

They as a whole reached high amphibolite facies to granulite facies with characteristic equilibrium assemblage of peak stage Sil+Grt+Bt±Crd+Kfs+Pl+Qtz.

荆山群变质岩系经历了三幕变形、六幕变质重结晶作用,峰期形成Sil+Grt+Bt±Crd+Kfs+Pl+Qtz特征平衡组合,变质程度达高角闪岩相-麻粒岩相。

During geological mapping of Xainza County in 2000, Tetragraptus approiimatus, the typical one of graptolite belts which cosmepolitically distributed in the Arenigian of Early Ordovician, was collected from the so-call Pre-Sinian Nianqingtanggula Group. So there is developped the Early Ordovician sediments and we have established Zakang Formation and Taduo Formation which perfected the Plaeozoic sequences in northern Tibet.

申扎地区1/25万区域地质调查工作中,在原归属为前震旦系念青唐古拉群的一套浅变质岩中发现了世界性分布的下奥陶统阿雷尼格阶最底部笔石化石带代表分子Tetragraptusapproximatus,首次确定了藏北地区有早奥陶世沉积地层的存在。

Near the contact boundary there exists a kind of metamorphic rock known as hornfels. It is resulted from the contact metamorphism when magma comes in contact with the sedimentary rocks and heats and squeeze s them.

在二者接触界线附近发育着一种叫角岩的变质岩,角岩的形成是由于岩浆人侵与周围沉积岩接触时所产生的热量和压力致使原岩发生变化而成。

Near the contact boundary there exists a kind of metamorphic rock known as hornfels. It is resulted from the contact metamorphism when magma comes in contact with the sedimentary rocks and heats and squeezes them.

在二者接触界线附近发育着一种叫角岩的变质岩,角岩的形成是由于岩浆人侵与周围沉积岩接触时所产生的热量和压力致使原岩发生变化而成。

Near the contact boundary there exists a kind of metamorphic rock known as hornfels. It is resulted from the contact metamorphism wh magma comes in contact with the sedimentary rocks and heats and squeezes them.

在二者 接触界线附近发育着一种叫角岩的变质岩,角岩的形成是由于岩浆人侵与周围沉积岩接触时所产生的热量和压力致使原岩发生变化而成。

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