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The Zijinshan copper-gold deposit is the high-sulphur epithermal deposit,which is characterized by both the high argillaceous alteration of dickite and alunite and the copper mineral association of enargite, digenite and covellite.

紫金山高硫浅成低温热液型铜金矿床以一套独具特色的由地开石、明矾石组成的高级泥质蚀变和由硫砷铜矿、蓝辉铜矿、铜蓝组成的铜矿物组合为特征。

Early Cretaceous granitic volcanic-intrusive complex in Xiushanlinchang of northeastern Da Hinggan Mt. consists mainly of rhyolite, rhyolite ignimbrite-trachytic dacite, trachyandesite formed in eruptive cycle stage and adamellite porphyry-geode syenogranite-graphic alkali feldspar syenogranite formed in hypabyssal invasion stage.

大兴安岭东北部秀山林场一带的早白垩世花岗质火山-侵入杂岩体由喷发旋回期的流纹岩、流纹质熔结凝灰岩-粗面英安岩、粗安岩和浅成侵入期的二长花岗斑岩-晶洞正长花岗岩-文象碱长正长花岗岩构成。

Jianchaling gold deposit belongs to the epithermal low temperature hydrothermal deposit with the auriferous mineralization strongly associated with the ultra basic rock,and the fault F 45 1 is acknowledged as main controlling structure.

煎茶岭金矿床是属于与超基性岩有密切成因关系的浅成低温热液型矿床,主控断裂为 F4 51 ,与 F4 51 断裂相关的次级断裂和张性裂隙构造是最重要的容矿构造。

Stamens 5 or rarely 4; filaments short; anthers mostly sagittate, free or connivent into a cone adherent to pistil head, dehiscing longitudinally, base rounded, cordate, sagittate, or prolonged into an empty spur; pollen granular; disc ringlike or cup-shaped, 2-5-lobed, or absent.

雄蕊5或很少4;花丝短花药多数箭头形,离生或靠合花柱成圆锥形,纵裂,基部圆形、心形、箭头形,或延长为空的距;花粉颗粒状;杯状的花盘环形或,浅裂的2-5,或无。

While the direct metallogenic environment is epithermal fluid evolution system.

而直接的成矿环境为浅成低温水热流体的成矿演化体系。

However, it shows also some phenomena of epithermal ore deposit, such as typical chemical composition of epitherm...

但同时,它的元素组合和围岩蚀变又显示出浅成热液矿床的某些特点。

Also,it is an important area of epithermal gold ore-deposits localities.

东南亚地区地处西太平洋构造-岩浆活动带上,是中新生代以来地球岩石圈中最复杂的构造活动区之一,也是全球浅成低温热液金矿床的重要产区之一。

As one of important type of gold deposits,the exploration and genesis research of epithermal gold deposits obtained some new advances recently.

浅成低温热液金矿床是一种重要的金矿类型,近年来其找矿勘查和成因理论研究取得了很大的进展。

Based on ore-bearing host rocks and mineralization patterns of copper-gold deposits in the western Tianshan Mountains, copper deposits can be classified into three types, i.

根据铜金矿床的含矿主岩和成矿作用方式,西天山的铜矿床主要可划分为 3种类型:斑岩型、夕卡岩型和火山热液型;金矿床可划分为 2种类型:浅成低温热液型和斑岩型。

Southeast Asia ,being a part of the Circum- Pacific tectono- magmatic belt,is one of the most complex tectonically active regions since the Mesozoic.

东南亚地区地处西太平洋构造-岩浆活动带上,是中新生代以来地球岩石圈中最复杂的构造活动区之一,也是全球浅成低温热液金矿床的重要产区之一。

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