摘要
新疆坡北-笔架山位于北山裂谷带内,发育较复杂的地层、构造和岩浆岩,该地区是新疆铜镍矿重要成矿远景区。该区与基性-超基性岩型有关的铜镍矿床有:坡十铜镍矿床、坡一铜镍矿床、红石山铜镍矿床等。通过对区域成矿地质背景、典型矿床特征、成矿规律总结,建立与基性-超基性岩有关的铜镍矿矿床成矿模式及区域成矿模式。
Pobei-Beacon Hill area is an important metallogenic prospective areas of Nickel-Copper ore in Xinjiang.It is located in the Beishan rift zone,forming complex stratigraphy,tectonic and magmatic rocks. There are Nickel-Copper de-posits related to mafic-ultramafic,such as Poshi Nickel-Copper deposit,Poyi Nickel-Copper deposit,Red Rock Hill Nick-el-Copper deposit,etc.Established Nickel-Copper ore deposits and regional metallogenic model related to mafic-ultramaf-ic after summarized the regional geological background,typical mineral characteristics and metallogenic regularity.
出处
《新疆地质》
CAS
CSCD
北大核心
2013年第2期184-189,共6页
Xinjiang Geology
基金
新疆维吾尔自治区1:5万区域地质矿产调查(XJQDZ2003-10)项目
新疆地质勘查基金(T10-3-24)项目联合资助
关键词
坡北-笔架山
基性-超基性岩
铜镍矿
成矿规律
Pobei-Beacon
Hill
Mafic-ultramafic
Nickel-Copper
Deposit
Geological
Background
Typical deposits
Metallogenic regularity
