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This stage orogenics may result from the collision of North Dabie micro-plate and North China plate, and result in the form of Sujiahe cold eclogite.

这一期的造山作用可能缘于北大别微陆块与华北板块之间的碰撞对接,并形成了苏家河榴辉岩。

The Hongqiling magmatic Cu-Ni sulfide deposit represented by No.1 and No.7 intrusions belongs to a typical magmatic liquation deposit in Xing'an-Mongolia orogenic belt.

以1号和7号岩体为代表的红旗岭铜镍硫化物矿床,是兴蒙造山带中典型的岩浆熔离型矿床。

They were formed in environment of late orogeny of active continent margin arc.

第二期侵入岩也为I型花岗岩,是具有壳幔混源特征的地壳物质深熔的产物,形成于活动大陆边缘弧晚造山环境之中。

Honghuapu intrusions in the west segment of Northern Qinling Mountains are dominated by tonalite with medium-fine-granular structure, which carry the geochemic characteristics of subduction-related granitic rocks.

北秦岭造山带西段红花铺侵入体的岩石类型为中细粒英云闪长岩,具俯冲型花岗岩类的地球化学特征。

In summary, it is evident that orogenic lode-gold deposits, hosted both in Precambrian greenstone belts and Precambrian to Phanerozoic accretionary sedimentary belts, commonly show predictable and repetitive structural geometries.

总之,很显然,赋存于前寒武纪绿岩带和前寒武纪到显生宙增生沉积带造山带脉金矿床,普遍表现出可预测的和重复的几何结构。

The albitite dispersed over the Qinshan_Zhulinguan area consists of a series of small intrusive and metasomatic bodies disintegrated from the "Jiuliping Formation" which is sandwiched between Zhulinguan-Qinshan fault and Shanyang-Doufujian fault in the East Qinling orogenic belt.

经1/5万区调填图,作者在东秦岭造山带夹持于竹林关-青山断裂带和山阳-豆腐尖断裂带之间的原划&九里坪组&地层中解体出了一系列规模不大的钠长岩体。

Part of the oceanic crust. The presence of the oceanic harzburgite in continental-type UHP belt reveals an integrated process of

地幔橄榄岩,从而揭示大陆造山带从早期的大洋俯冲消亡到大陆俯冲碰撞的完整过程。

In accordance with the characteristics of the occurence and tectonic emplacement of the ophiolitic belt.

目前认为蛇绿混杂岩带是洋盆闭合时洋壳残片构造侵位到陆壳之中的产物,为无序层序,相当于造山带非史密斯地层学划分类型的构造混杂体类,即由构造包体和基质两大部分组成。

Type I is composed of rhyolitic rocks, which are characterized by higher Si and alkali contents and lower Al and Ti contents, Na2O/K2O1 and a weak negative Eu anomaly (δEu=0.65–0.95), enriched in Sr and Ba and poor in Rb. Types I and II probably formed in an extensional to postorogenic extensional environment, accompanied by compressional uplift.

提要:大兴安岭北段根河地区早白垩世火山杂岩按岩石及其地球化学特征,可划分为3类:第Ⅰ类为流纹质岩石,富Si,碱,低Al,Ti,Na2O/K2O1,具弱的负Eu异常(δEu=0.65~0.95),富Sr,Ba,贫Rb;研究认为第Ⅰ,Ⅱ类岩石产于挤压隆升相伴的拉张至造山后伸展构造环境。

Study and application on reservoir sensitivity of Baimiao gas condensate field ;2. Yangtake gas condensate field exists a suit of composite salt bed in Eogene system,in which interspersing soft mudstones.

羊塔克凝析气田位于塔北隆起羊塔克构造带1号构造东端,下第三系普遍存在一套复合盐岩层,特别是夹在复合盐岩层中的软泥岩、复合盐膏层缩径与井漏并存,造成井眼极不稳定,给钻井施工带来很多复杂和事故,其钻井风险很大,尤其是216mm井眼的电测和下套管作业更是异常困难。

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