基本释义:

太古代绿岩带

网络释义

1)Archaean greenstone belt,太古代绿岩带

2)Late Archean greenstone belt,晚太古代绿岩带

3)Archaean greenstone belt type gold deposit,太古代绿岩带金矿

4)greenstone belt of Archaeozoic era,太古宇绿岩带

5)Archean greenstone belt,太古宙绿岩带

6)Archean granite-grenstone belts,太古窗花岗岩-绿岩带

用法和例句

They have the typical geologic features of the golddeposits of Archean greenstone belt.

山西五台山太古宙绿岩带同构选初生型金矿床发现三种类型：条带状铁建造型。

Connemara gold deposit is associated with Archean greenstone belt and Precambrian metamorphic rocks.

康尼玛拉金矿床的形成与太古宙绿岩带、前寒武系变质岩关系密切,矿体、矿化蚀变体主要受NNW向断裂构造控制,属破碎蚀变岩型金矿,围岩蚀变发育,硅化、黄铁矿化、绢云母化与矿化关系密切,该矿区具有良好的找矿前景。

Evaluation of Anomalies of Dispersion Trains of Cu-Zn Deposits in Archeozoic Greenstone Belt, Qingyuan, Liaoning

清原地区太古代绿岩带铜锌矿床分散流异常的评价方法

Unit two belongs to late Archaean middle-low grade metamorphic rocks with the characteristics of granite -greenstone belt.

组合(2)是具花岗—绿岩带特征的晚太古代中、低级变质岩系.

The Archaean meta-basalts are distinguished into two meta-basalts formed in the greenstone belt and in the high-grade metamorphic region.

本文把太古代变质玄武岩分成绿岩带变质玄武岩和高级区变质玄武岩。

LATE ARCHAEAN GREENSTONE BELT IN ZHIFANG AREA, TAIAN, SHANDONG, AND THE CHARACTERISTICS OF THE GOLD MINERALIZATION THERE

山东泰安纸房地区太古代晚期绿岩带及其金矿化地质特征

The early Precambrian in Jilin province includes the Archaeozoic granite-greenstone belt,early Proterozoic Ji’an Group and mid Proterozoic Laoling Group .

吉林省早前寒武纪地质包括太古宙花岗—绿岩带、早元古代集安群和中元古代老岭群。

METALLOGENIC CHARACTERISTICS OF IRON DEPOSITS IN ARCHEAN GREENSTONE BASIN OF ANSHAN-BENXI AREA, NORTHEAST CHINA

鞍本太古代绿岩盆地铁矿的成矿特征

Archean Era Greenstone Bel Gold Deposit of Ore-Hunting Evidence in Middle Part Inner Mongolia

内蒙古中部地区太古宙绿岩带金矿找矿标志

The REE Geochemistry of Granitic Rocks in Qingyuan Archean Greenstone-Granite Terrene

清原太古代花岗—绿岩区花岗岩的稀土地球化学

A SIMPLE DISCUSSION ON METALLOGENIC SYSTEM OF GOLD DEPOSITS IN WUTAISHAN ARCHEAN GREENSTONE BELT OF SHANXI

山西五台山太古宙绿岩带金矿成矿系统初论

THE METALLOGENTIC CHARACTERISTICS OF GOLD DEPOSITS OF THE ARCHEAN GREENSTONE BELTS IN NORTH CHINA PLATFORM

华北陆台太古宙绿岩带金矿的成矿特征

A PRELIMINARY STUDY ON STRATABOUND CHARACTERISTICS OF THE GOLD DEPOSITS IN ARCHAEAN GREENSTON IN SOUTHERN JILIN AND NORTHERN LAONING

吉南辽北太古代绿岩金矿层控特征的探讨

GEOLOGY AND GEOCHEMISTRY OF ARCHEAN GRANITE-GREENSTONE BELTS IN NORTHERN LIAONING PROVINCE AND SOUTHERN JILIN PROVINCE

辽北－吉南地区太古宙花岗岩－绿岩带地质地球化学

DEFORMATION OF OPHIOLITIC MELANGE OF LATE PALAEOZOIC IN NORTH TIANSHAN OF XINJIANG

新疆北天山晚古生代蛇绿混杂岩带的变形研究

THE DOWNWARD MIGRATION OF GOLD INTO THE DEEP ARCHEAN GREENSTONE BELT AND ITS PRECONCENTRATION:TAKING THE TAIHUA GROUP IN SHAANXI AND HENAN PROVINCES AS AN EXAMPLE

太古宙绿岩带金的“下迁预富”作用─—以豫陕太华群地层为例

MAJOR AND TRACE ELEMENT GEOCHEMISTRY OF THE ARCHEAN QINGYUAN GRANITE-GREENSTONE TERRANE

清原太古代花岗岩-绿岩地体的常量和微量元素地球化学证据

Studies of Garnets from the Archean Metamorphic Complex in Liaoxi (Weat Liaoning)-Chifeng Area

辽西—赤峰—带太古代变质杂岩中石榴石的研究

GEOLOGICAL CHARACTERISTICS AND MINERALIZAINGMECHANIZM OF PYRITE DEPOSITS IN ARCHAEAN GREENSTONE BELT IN THE WESTERN SHANDONG REGION

鲁西地区太古宙绿岩带硫铁矿床地质特征及成矿机制

Qing-Yuan district is a granite-greenstone terrain, The greenstone was formed during the youth stage of massif rifting in late Archean.

清原地区是一个花岗——绿岩区,绿岩是在晚太古代年轻地体裂谷期形成。