摘要
该区属特提斯成矿域中南半岛成矿带,是印度尼西亚金储量最为丰富的金多金属矿成矿带。申请区位于中南半岛成矿带的东南段,是纲瓦纳大陆分离北移部分,在古生代末及中新生代初遭受多期次构造-岩浆作用的叠加改造。该成矿带主要矿产有金、银、铅锌、钾盐等。该区是东西向的班达亚岩浆弧一部分,区域构造总体上形成NE-SW向和NW-SE向断裂控制的菱形网格状构造形迹。从新近纪到渐新世晚期持续发生岩浆的侵入及火山喷发活动,区域性断裂极其派生的次级构造为金多金属矿形成提供了有利的条件。该区属特提斯成矿域中南半岛成矿带,是印度尼西亚金储量最为丰富的金多金属矿成矿带之一。龙目岛西部金矿选区位于印度尼西亚金资源储量最多的金多金属成矿带上。通过对前人地质资料的综合研究和分析,并到实地踏勘研究认为,该区成矿条件优越,以金矿化为主。该区是寻找构造蚀变岩型金矿的最有利部位。
the ringed mountains belongs to tethys metallogenic domain south peninsula metallogenic belt, is Indonesia gold reserves the mos! rich goht polymetallic metallogenic belt. Application area is located in the southeast of metallogenic belt in the [ndochina peninsula section, is Ihe steel tile accept mainland separation north shift part, in the early Paleozoic and Cenozoic suffered many times strueture-magmatism superpesitinn and transformation. The metallogenie belt main mineral have gold, silver, lead and zinc, potassium, etc. The area is east-west banda and magmatic are part, regional structure on the whole form to NE-SW and NW-SE to fracture control diamnnd mesh structure shows. From neogene to late Oligocene ongoing magma intrusion and volcanic eruption activities, regional fracture is derived secondary structure for gold polymetallic deposit formation provides favorable conditions. The tinged mountains belongs to tethys metallogenic domain south peninsula metallogenie belt, is Indonesia gold reserves the most abundant oue of gold polymetallic metallogenic belt. Lombok western gold mine district is located in Indonesia gold resources reserves the most gold polymetallic mineralization take. Based on previous geological data comprehensive research and analysis, and to the field reonnaissance research thinks, the metallogenic condition is superior, to give priority to gold mineralization. The area is looking for tectonic altered rock type gold ore is the most favorable position.
出处
《科技视界》
2016年第2期264-264,285,共2页
Science & Technology Vision
关键词
成矿带
构造
多金属
火山喷发作用
Metallogenic belt
Structure
Metal
Volcanic eruption
