The ductile shear zone type gold deposits refer to those whose ore-forming mechanism and ore-controlling factors are closely related to the ductile shear zone and its evolution. Different ductile shear zones are well devel-oped in the northern Altun area. The controls of ductile shear zone on gold deposits are as follows. (1) The re-gional distribution of gold deposits (and gold spots) is controlled by ductile shear zones. (2) The ductile-brittle shear zones formed in the evolution process of ductile shear zones both are as only ore-bearing structures and control the shape, attitude, scale and distribution of mineralization zones and orebodies. (3) The mechanical property of compression-shear ductile deformation determines that the main kind of gold mineralization is the al-tered mylonite type and main alteration is metasomatic. (4) Ore-bearing fracture systems are mainly P-type one and secondarily D-type and R-type ones, in adition R'-type and T-type one in one or two cases. (5) Dynamic differentiation and dynamic metamorphic hydrothermal solution resulting from ductile deformation is one of the sources of gold ore-forming fluids. And this is consistent with the idea drawn from the feature of fluid inclusion and geochemical characteristics of the deposit, i. e. ore-forming material resources are mainly from metamorphic rocks and ore-forming fluids are mainly composed of metamorphic water. (6) There is a negative correlation be-tween the gold abundance and susceptibility anisotropy (P) of the altered mylonite samples from the deposits, which shows that the gold mineralization is a little later than the structural deformation. All above further ex-pound the ore-forming model of the ductile shear zone type gold deposits.