1.
FEATURES AND GENESIS OF THE URANINM-MINERALIZED BRECCIA IN EAST QINLING
东秦岭某地铀矿化角砾岩特征和成因
2.
Gold-hosted breccia in Shuangwang ore deposit is hydrofracturing breccia.
双王金矿含金角砾岩水力压裂成因角砾岩。
3.
Discussion on Searching for the Latent Explosion of Breccia Mineral Deposit in Fujian Ancun Mining
福建安村矿区寻找隐爆角砾岩矿床的探讨
4.
GEOLOGICAL CHARACTERISTICS AND ORE-CONTROLLING SIGNIFICANCE OF THE CRYPTOEXPLOED BRECCIA IN NIUJUAN SILVER DEPOSIT,IN HEBEI PROVINCE
河北牛圈银矿隐爆角砾岩地质特征及控矿作用
5.
The host rock conformably overlies a band of siliceous chertybrecia.
含矿主岩整合地上覆于硅质燧石角砾石带之上。
6.
Enrichment Regularity of Gold in the Qiyugou Explosive Breccia Type Gold Deposits, Henan Province
河南祁雨沟爆发角砾岩型金矿床金的富集规律
7.
Discussion on the Genesis and Prospecting Direction of Cryptoexplosive Breccia Type Deposit in Case of Laotian Rockmass
从老田岩体谈隐爆角砾岩型矿床的成因机制和找矿方向
8.
Low Dip Ore-forming Theory of Cryptoexplosive Breccia Deposit and Its Application
隐爆角砾岩型矿床矿体缓倾斜成矿理论及其应用
9.
To form(rock) into breccia.
使（岩石）形成角砾岩
10.
The Formation of Breccia and Ore Body's Localization Mechanism in Fenghuangshan Copper Deposit,Tongling Area,Anhui Province,China
铜陵凤凰山铜矿床角砾岩的形成与矿床定位机制
11.
Breccia-Vein System of Liuqiong Hot Spring Type Gold Deposit,Guangxi: Characteristics and Genesis
广西六琼矿区热泉型金矿床网脉-角砾岩特征及其成因探讨
12.
THE PROSPECTING SIGNIFICANCE AND THE ORIGIN OF BRECCIA IN THE LOWER PART OF MANTOU FORMATION OF THE LOWER CAMBRIAN SYSTEM IN WESTERN LIAONING AREA
辽西地区下寒武统馒头组下部角砾岩的成因及其找矿意义
13.
BASIC CHARACTERISTICS OF PRIMARY HALOS IN THEQIYUGOU EXPLOSION BRECCIA TYPE GOLD DEPOSIT,HENAN PROVINCE
河南祁雨沟爆发角砾岩型金矿床原生晕基本特征
14.
Alteration and the Forming Dynamic Process of the Qiyugou Breccia Gold Deposit;
祁雨沟角砾岩型金矿蚀变类型及其形成的动力学过程
15.
The Tectonic Genetic Model of Gold-bearing HydrofracturingBreccia Body and Control of Gold Ore Body in the shuangwangGold Deposit ,Shanxi Province;
陕西双王含金水压角砾岩体构造成因模型及其对金矿的控制
16.
Compositions of the Kimberlitic Brecciated Peridotite in the Bachu Area,Xijiang and Its Ore-Bearing Potentialities
新疆巴楚地区金伯利质角砾橄榄岩物质组成及含矿性研究
17.
The characteristics of fault karst breccia are the combination of fault breccia and karst breccia. It is a product of fault actions and karst collapses.
断溶角砾岩兼具断层角砾岩和岩溶角砾岩的特点,是断裂和岩溶塌陷共同作用的产物。
18.
The article introduces the distributing area, thickness change, the old river erosion and sediment surroundings of conglomerate layer K21.
就大同矿区K21砾岩层的分布范围、度变化、河流冲刷现象、砾径变化、积相等进行了介绍。