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中畈金矿区域上位于扬子地台东南缘的江南古陆北部边缘,七都复式背斜北翼三岗尖—杨田背斜西端核部,东至—石门街断裂西侧,江南深大断裂南侧。沿黄栗树—东至一线以北地区主要出露古生代地层,以南主要为震旦系和中元古代地层(陈寿椅等,2012)。地层总体走向北东,倾向北西、南东,由南向北地层自老而新。区域上构造复杂、多期,主要表现为褶皱及断裂构造。主要褶皱有中畈—东至背斜、高村—戴村向斜、许村背斜,分别属七都复式背斜北
The Zhongli gold deposit is located on the northern edge of the southern Yangtze paleosol in the southeastern margin of the Yangtze Platform. The northern part of the Qidou anticlinorium is located at the west end of the Sangangjian-Yangtian anticline, to the west of the Yangtian anticline, to the west of the Shihmenjie fault, South of the fault. Along the Yellow Chestnut - the area to the north of the east to the first line, mainly Paleozoic strata are exposed, while the south mainly consists of Sinian and Mesoproterozoic strata (Chen Shouchi et al., 2012). The strata generally go to the east, northwest and south east, and the strata from south to north are old and new. The structure is complex and multi-period in the area, mainly showing folds and faults. The main folds of the Central Plains - the east anticline, high village - Dai Village syncline, Xucun anticline, respectively, are seven arequito anticlinal