内蒙古1∶25万柴河镇（L51C001001）、蘑菇气（L51C001002）幅区调修测项目（1212011120654） 及国家自然科学基金(40972059) 联合资助。
Abstract：Ore-controlling structure is always one of the difficulties in the study of hydrothermal deposits. With Chaihezhen-Moguqi region of the Da Hinggan Mountains as the study object, this paper puts forward some conclusions on the basis of the 1:250000 geological investigation of. Chaihezhen-Moguqi region. 1. The main ore-controlling structures are Daheishan-Taipingling-Jiguanshan fracture zone and Zalantun City-Haduo River fracture zone, and the formation ages are mainly Hercynian and Yanshanian. 2. Ore-controlling structures mainly show compression, tensile and shear properties, and between the three properties, there existed the conversion between shear and tensile and between shear and torsion, with the principal compressive stress field changing in the directions of E-W, SE-NW to SSE-NNW in succession. 3. The regularities of the main ore-controlling structures, the branching ore-control structures, and the parallel and inclined ore-controlling structures are summarized in this paper. These regularities, the structures as passageways for ore fluids and the ore source were closely related to deep subduction which produced molten magma. These new ideas are of great significance for the detailed study of geological foundation, metallogenic theory and prospecting work in this region.
孙忠实 刘四川 郑常青 谭 亮 孙 黎 李 娟 施 璐 崔芳华 范思琦. 大兴安岭柴—蘑地区控矿构造特征及赋矿规律[J]. 中国地质, 2013, 40(2): 529-537.
SUN Zhong-shi, LIU Si-chuan, ZHENG Chang-qing, TAN Lian, SUN Li, LI Juan, SHI Lu, CUI Fang-hua, FAN Si-qi. The ore-control structural features and ore-host regularity of Chaihe-Moguqi area in the Da Hinggan Mountains[J]. Geology in China, 2013, 40(2): 529-537(in Chinese with English abstract).