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Niushan downtown area is rich in structure, a lot of points around the mine, mineralization is closely related with the structural characteristics. In this paper, by analyzing the downtown Niushan regional geological background, structural characteristics and the relationship between structure and mineralization, combined with junior internship in the area of production of the field survey results, that the area affected by the NNE Daxinganling Nenjiang deep fault and the main ridge deep fault long-term activities, formation of the Early Cretaceous in the area East and West, North East and North West to the three major faults, have shown that torsional fault pressure characteristics, body parts given the existence of fault intersection.
NW-NE-trending fault intersection control area to the NW part of the direction of the volcano jet dump bodies; downtown Niushan multi-layer ring-shaped structure confining the downtown Niushan volcanic dome-shaped body, with a ring-fault system, the ring interface layer are lots more broken rock strata.
Distribution of ore bodies with the fracture, fracture zone, and constitute a more ore to the group. EW to, NW-trending fault, as well as multi-layer ring-like circular structure geophysical and geochemical anomalies for the area, downtown Niushan copper-polymetallic mineralization, as well as rock - such as aspects of structure have a direct and indirect control.
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Noisy cattle mountain area structure phenomenon enriches , the periphery ore counts many, become the ore and the structure characteristic going hand in hand. The main body of a book is concerned by analysing noisy cattle mountain area area geology background , structure characteristic and structure and ready-made an ore's , is is tied in wedlock the big three turn out practice open country result to that area, think that area accepts the north north east fracture to Nen Jiang depths and flexible effect of very much tearing long range of the Great Xing'an Mountain host spine, world formation should area thing , the north east and the north west in early chalk to three big fracture, demonstrate pressure equally twisting the fault characteristic, location there existing the tearing relationship in ore body tax converging. NW-NE converges to tearing relationship location controls the volcano organization being area's turn to incline to NW direction gushing; Noisy Niushanduo tier of shapes annularity structure is surrounded being restricted to noisy Niu Shan dome shape volcano organization , is have tearing system of cyclic annular, that every is encircled by tier of interfaces is more broken rock rock stratum section of an area equally. The ore body stretches cloth and these break , break to pieces as well as being connected with, ore body composing the multiway group. EW all has direct and indirect control action tier to NW, to break and multilayer shape annularity structure outside ring to being area materialization's turn to explore abnormal , noisy Niu Shan copper all aspect such as much metal mineralization and rock mass- structure.

Niushan downtown area is rich in structure, a lot of points around the mine, mineralization is closely related with the structural characteristics. In this paper, by analyzing the downtown Niushan regional geological background, structural characteristics and the relationship between structure and mineralization, combined with junior internship in the area of production of the field survey results, that the area affected by the NNE Daxinganling Nenjiang deep fault and the main ridge deep fault long-term activities, formation of the Early Cretaceous in the area East and West, North East and North West to the three major faults, have shown that torsional fault pressure characteristics, body parts given the existence of fault intersection.
NW-NE-trending fault intersection control area to the NW part of the direction of the volcano jet dump bodies; downtown Niushan multi-layer ring-shaped structure confining the downtown Niushan volcanic dome-shaped body, with a ring-fault system, the ring interface layer are lots more broken rock strata.
Distribution of ore bodies with the fracture, fracture zone, and constitute a more ore to the group. EW to, NW-trending fault, as well as multi-layer ring-like circular structure geophysical and geochemical anomalies for the area, downtown Niushan copper-polymetallic mineralization, as well as rock - such as aspects of structure have a direct and indirect control.

The noisy cow mountain area structure phenomenon is rich, the peripheral mineralization point are many, the mineralization and the structure characteristic are closely related. This article through analyzes the noisy cow mountainous region trivial territory geology background, the structure characteristic and the structure and the mineralization relations, unifies the big three productive practice to this area open country survey result, thinks this area the north north east to the Nenjiang River deep fracture and Greater Hinggan Mountain main keel deep fracture long-term activity influence, in the early chalk world forms this area thing, north east and north west the direction three big breaks, demonstrated that the pressure wrenches apart the level characteristic, the ore body bestows on the existence break connection spot. NW-NE controls this area to the break connection spot the volcano organization which spurts to the NW side incidence; Noisy Niu Shanduo the layered ring structure encircles is limiting the noisy cow mountain dome-shaped volcano organization, has the ring-like break system, various lamellars contact surface is the rock rock layer stave land sector. ore body mop and these breaks, crushed zone related, constitution multi-direction group ore body. EW to, NW as well as outside the layered ring structure the lamellar searches exceptionally, noisy Niu Shantong to the break regarding this area transformation the polymetallic mineralization as well as the rock mass - structure and so on various aspects has direct and the indirect control action

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