中亚成矿域斑岩铜（钼）矿带的认识与建立

Knowledge of porphyry Cu (Mo) ore belts in the Central Asian metallogenic domain and their establishment

1.
Xinjiang Geological Survey, China Nonferrous Metals Geological Survey Center, Urumqi 830011, Xinjiang, China
2.
China Nonferrous Metals Geological Survey Center, Beijing 100012, China

摘要: 提要：对中亚成矿域斑岩铜（钼）矿带的认识，起源于哈萨克斯坦滨巴尔喀什—伊犁火山侵入岩带的划分和地球物理场的确认。尤其是对哈萨克斯坦—准噶尔环状磁力异常带的厘定，奠定了中亚成矿域斑岩铜（钼）矿带的地球物理基础和与哈萨克斯坦—准噶尔地块外缘火山-侵入岩带的耦合关系，最终建立起哈—中—蒙中亚成矿域斑岩型铜（钼）矿带的雏型。
- 斑岩型铜（钼）矿带 /
- 中亚成矿域 /
- 认识
Abstract: Abstract：Knowledge of the porphyry Cu (Mo) ore belts in the Central Asian metallogenic domain originates from the division of the peri-Balkhash-Ili volcanic-intrusive belt in Kazakhstan and confirmation by the geophysical field. Through the definition of the Kazakhstan-Junggar ring-shaped magnetic anomaly zone, the authors lay a geophysical foundation of the porphyry Cu (Mo) ore belts of the Central Asian metallogenic domain and recognize their coupling relation to the volcanic-intrusive belts at peripheries of the Kazakhstan-Junggar block. On that basis, an embryo of the porphyry Cu (Mo) ore belts in the Kazakhstan-China-Mongolia Central Asian metallogenic domain is established.
- porphyry Cu (Mo) metallogenic belt /
- Central Asian metallogenic domain /
- undefined