Abstract：Based on the special geomorphology of basin-ridge structure, complex structural intersection, inheritance and continuity of multi-stage NW- and N-S-trending ore-forming structures, the control of Mesozoic granite belt and volcanic rock zone on mineralization and the unique structural trend of NW-runing geophysical anomaly, the authors confirm the existence of NW-trending tectonic-metallogenic belt on the right bank of Heilongjiang River. Many deposit examples indicate that the multi-stage NW-trending tectonic belt has several metallogenic functions like rock-controlling, ore-controlling, ore guide and host. The horizontal zonation of deposits/orebodies is obvious, which provides theoretical basis for exploration prediction on the right bank of Heilongjiang River.
杨继权, 杨钦. 论黑龙江右岸北西向构造带的确立及其对成矿的控制作用[J]. 地质与资源, 2015, 24(5): 428-432.
YANG Ji-quan, YANG Qin. CONFIRMATION OF THE NW-TRENDING TECTONIC BELT ON THE RIGHT BANK OF HEILONGJIANG RIVER AND ITS CONTROL ON MINERALIZATION. GEOLOGY AND RESOURCES, 2015, 24(5): 428-432.
2015, Vol. 24 
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