ID,DEPOSIT NAME,TECTONIC SETTING,REGIONAL GEOLOGY,,,,,,,,,,,
1,Amangshaji,--,--,,,,,,,,,,,
2,Anjiacha,--,--,,,,,,,,,,,
3,Badu,--,--,,,,,,,,,,,
4,Badun,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
5,Baguamiao,south of Qinling transform zone,"Sujiagou-Kuonggua multiple syncline, with tight folds and faults trending northwest",,,,,,,,,,,
6,Baidi,Same as RE00789,Same as RE00789,,,,,,,,,,,
7,Baihe,--,--,,,,,,,,,,,
170,Bancanggou,--,--,,,,,,,,,,,
8,Bannian,Same as RE00789,at south of Laizishan short axial anticline,,,,,,,,,,,
9,Banqi,near buried southwestern margin of Precambrian Yangtze craton,along southern edge of small (15-km-long) east-west trending dome that has Permian Houziguan limestone exposed in center,,,,,,,,,,,
10,Baqiao,--,--,,,,,,,,,,,
11,Baxi,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
171,Beiya,Ailao mountain low pressure metamorphic belt,Jinchang gold lode zone trending north-south is found at west of the ultrbasic intrusions,,,,,,,,,,,
12,Beiyinpo,Same as RE00789,controlled by Huijiapu anticline which trend east to west,,,,,,,,,,,
13,Ceyang,near buried southwestern margin of Precambrian Yangtze craton,"at southern end of 30 km-long Lugong anticline, which exposed Permian rocks along crest; Axis of anticline trends north-south, parallel to margin of Yangtze craton and to strike of faces changes",,,,,,,,,,,
14,Chabu,western Qinling transform zone,Bailongjiang gold belt is about 160 ~ 200 km long and trends east to west. It is distributed along with Bailongjiang thrust zone. Gold mineralization occurs in a black formations of Cambrian and Devonian,,,,,,,,,,,
15,Chaijiaping,--,--,,,,,,,,,,,
16,Changkeng,southwest margin of Yangtze craton & Hunan fold system,"Sanzhou basin is located at intersection of Enping-Cong faults zone, trending northeast, and Gaoyiao-Huilai faults zone, trending east-west",,,,,,,,,,,
17,Chanziping,--,--,,,,,,,,,,,
18,Dachang,southwest margin of Yangtze craton,two graben faults in this area trend northeast and northwest,,,,,,,,,,,
19,Daguan,Same as RE00789,Same as RE00789,,,,,,,,,,,
20,Damingshan,"Dian-Qian-Gui district is located near buried southwestern margin of Precambrian Yangtze craton, among Kangdian, Yuebei and Jiangnan old lands","Youjiang rift valley, which trends northwest, is a regional ore-control structure in Dian-Qian-Gui area. With the development of Youjiang rift valley, ore-bearing formations, which are made up of alternative phases of shallow sea and land such as clastic,",,,,,,,,,,,
21,Daoqiejia,--,--,,,,,,,,,,,
22,Dashui,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
23,Dayakou,Same as RE00789,Same as RE00789,,,,,,,,,,,
24,Dazhai,--,--,,,,,,,,,,,
25,Dongbeizhai,west margin of Yangtze craton,near the intersection of west Qinling thrust folds belts trending west-east and Minjiang thrust folds belts,,,,,,,,,,,
26,Douyajing,--,--,,,,,,,,,,,
27,Erdaqiao,--,--,,,,,,,,,,,
28,Ertaizi,west Qinling transform zone,"deposit is on south of a multiple anticline, controlled by intersection of two sets of fault trending east-West and northeast",,,,,,,,,,,
29,Gala,west margin of Yangtze craton,Ganzi-Xianshuihe gold belt trending northwest,,,,,,,,,,,
30,Gaojiaao,intersection of Baimashan-Longshan magma-structural zone and Taojiang-Chengbu rift in Yangtze craton,"Lianhuazhai-Baiyunchuong dome formed by fault is major structure in the orefield, which trends northwest. Two sets of fault trending northeast and northwest are relative to gold deposit",,,,,,,,,,,
31,Gaolong,Same as RE00789,Same as RE00789,,,,,,,,,,,
32,Gedang,--,--,,,,,,,,,,,
33,Gejiebisu,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
34,Gengxin,--,--,,,,,,,,,,,
35,Getang,near buried southwestern margin of Precambrian Yangtze craton,"deposit located on eastern limb of Getang dome, a northwest-trending anticline about 50 km long; Permian rocks exposed at center of dome",,,,,,,,,,,
36,Greatwall,Locate in the Longkou Proterozoic sedimentary basin at northern margin of the Hubei craton,"Five stratabound breccia bodies,  trending NNW and 5-15 km long, control the gold mineralization.",,,,,,,,,,,
172,Guji,--,--,,,,,,,,,,,
173,Gulu,--,--,,,,,,,,,,,
37,Guohua,--,--,,,,,,,,,,,
38,Guojiapo,--,--,,,,,,,,,,,
174,Gutaishan,margin of Yangtze craton,"located in Proterozoic and Sinian silty argillite, sericite slate and siltstone",,,,,,,,,,,
39,Heduosi,western Qinling transform zone,Bailongjiang gold belt is about 160 ~ 200 km long and trends east to west. It is distributed along with Bailongjiang thrust zone. Gold mineralization occurs in a black formations of Cambrian and Devonian,,,,,,,,,,,
40,Hefei,--,--,,,,,,,,,,,
41,Hengxian,--,"Gold mineralization along a fault trending NE 70, which is a contact fault between Cambrian and Cretaceous strata.",,,,,,,,,,,
42,Heye,--,--,,,,,,,,,,,
43,Huachanggou,--,--,,,,,,,,,,,
175,Huameinao,"intersection of Tanlu rift and Huaiyang folds, Yangtze craton",tight close folds trending east-west were cut by igneous intrusion,,,,,,,,,,,
44,Huanglong,--,--,,,,,,,,,,,
45,Huangshan,--,--,,,,,,,,,,,
46,Huangshi Laoshan,--,--,,,,,,,,,,,
47,Huangtupo,--,--,,,,,,,,,,,
48,Huayuangou,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
49,Hujiamo,--,--,,,,,,,,,,,
50,Jiangjuncha,--,--,,,,,,,,,,,
51,Jiaoguan,--,--,,,,,,,,,,,
52,Jiawuchi,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
53,Jidoman,--,--,,,,,,,,,,,
54,Jiguanzui,--,--,,,,,,,,,,,
176,Jiguanzui,"intersection of Tanlu rift and Huaiyang folds, Yangtze craton",tight close folds trending east-west were cut by igneous intrusion,,,,,,,,,,,
55,Jilongshan,"intersection of Tanlu rift and Huaiyang folds, Yangtze craton",tight close folds trending east-west were cut by igneous intrusion,,,,,,,,,,,
56,Jinba,--,--,,,,,,,,,,,
177,Jinchang,Ailao mountain low pressure metamorphic belt,Jinchang gold lode zone trending north-south is found at west of the ultrbasic intrusions,,,,,,,,,,,
57,Jinlongshan,west Qinling transform zone,a series of folds and faults which trend east-west,,,,,,,,,,,
58,Jinshan,west Qinling transform zone,"located at south of Zhongchuan granite, in Wujiazhuang outfold",,,,,,,,,,,
59,Jinya,--,--,,,,,,,,,,,
60,Jinyia,southwest margin of Yangtze craton,"slope zone of Lingyun dome uplift, northeast of fault valley; A series of folds go along with faults trending north-south",,,,,,,,,,,
61,Jinzhudong,--,--,,,,,,,,,,,
178,Jiucaigou,--,--,,,,,,,,,,,
62,Jiuyuan,western Qinling transform zone,Bailongjiang gold belt is about 160 ~ 200 km long and trends east to west. It is distributed along with Bailongjiang thrust zone. Gold mineralization occurs in a black formations of Cambrian and Devonian,,,,,,,,,,,
179,Kagu,--,--,,,,,,,,,,,
63,Kama,western Qinling transform zone,Bailongjiang gold belt is about 160 ~ 200 km long and trends east to west. It is distributed along with Bailongjiang thrust zone. Gold mineralization occurs in a black formations of Cambrian and Devonian,,,,,,,,,,,
64,Kangjiawan,--,--,,,,,,,,,,,
65,Laerma,west Qinling transform zone,faults zone trending east to west are main ore control structure in Maqu-Diebu thrust,,,,,,,,,,,
66,Langquan,--,--,,,,,,,,,,,
67,Lannigou,southwest margin of Precambrian Yangtze craton,"east wing of Laizi mountain short-axial anticline, southwest of the Banchang thrust trending northwest",,,,,,,,,,,
68,Laodou,--,--,,,,,,,,,,,
180,Laotiechang,--,--,,,,,,,,,,,
69,Lapu,--,--,,,,,,,,,,,
70,Lazikuo,western Qinling transform zone,Bailongjiang gold belt is about 160 ~ 200 km long and trends east to west. It is distributed along with Bailongjiang thrust zone. Gold mineralization occurs in a black formations of Cambrian and Devonian.,,,,,,,,,,,
71,Lianhecun,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
72,Liba,west Qinling transform zone,"intersection of rifts, which were produced ether by moving of ground blocks or igneous intrusions",,,,,,,,,,,
73,Lijiagou,middle of Qinling transform zone,"intersection of Qinling fold system and Lingtan-Shanyang fault. Devonian formation that is composed of slate, metamorphic siltstone and carbonate rocks is predominant in the area",,,,,,,,,,,
181,Linxiang,--,--,,,,,,,,,,,
182,Longchang,--,--,,,,,,,,,,,
74,Longchuan,--,--,,,,,,,,,,,
75,Longdishui,--,--,,,,,,,,,,,
76,Longhue,Same as RE00789,Same as RE00789,,,,,,,,,,,
77,Longna,Same as RE00789,Same as RE00789,,,,,,,,,,,
183,Longshan,margin of Yangtze craton,"located in Proterozoic and Sinian silty argillite, sericite slate and siltstone",,,,,,,,,,,
78,Longwanggou,--,--,,,,,,,,,,,
79,Longzhen,--,--,,,,,,,,,,,
80,Loudong,Same as RE00789,at north of Laizishan short axial anticline,,,,,,,,,,,
81,Lubuge,Same as RE00789,Same as RE00789,,,,,,,,,,,
82,Luoba,--,--,,,,,,,,,,,
83,LuoDa,--,--,,,,,,,,,,,
84,Luolou,--,--,,,,,,,,,,,
85,Maanqiao,--,--,,,,,,,,,,,
86,Maehan,--,--,,,,,,,,,,,
87,Mahuanggou,north margin of Yangtze craton,Houlongmenshan gold belt goes along the thrust and trends northeast. carbonate formation of Paleozoic exposed at southeast side and clastic formation of Triassic at northwest.,,,,,,,,,,,
88,Majiagou,--,--,,,,,,,,,,,
89,Manaoke,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
90,Maoling,Huabei craton (or north China platform),Yinkao-Kuandian subprovince near boundary with Fuzhao Subprovince of north China platform. the area is mostly underlain by Proterozoic sedimentary rocks and Mesozoic granites,,,,,,,,,,,
91,Maquan,west Qinling transform zone,"located at south of Zhongchuan granite, in Wujiazhuang outfold",,,,,,,,,,,
92,Mashan,--,--,,,,,,,,,,,
93,Maxuong,Same as RE00789,Same as RE00789,,,,,,,,,,,
94,Miaolong,southwest margin of Yangtze craton,Sandu-Danzhai gold belt trending north to south,,,,,,,,,,,
95,Mingshan,--,--,,,,,,,,,,,
96,Mingzhushan,--,--,,,,,,,,,,,
184,Mobing,margin of Yangtze craton,"located in Proterozoic and Sinian silty argillite, sericite slate and siltstone",,,,,,,,,,,
97,Mozigou,--,--,,,,,,,,,,,
98,Nabi,--,--,,,,,,,,,,,
99,Nanjing,--,--,,,,,,,,,,,
100,Nipu,Same as RE00789,Same as RE00789,,,,,,,,,,,
185,Panghe,--,--,,,,,,,,,,,
101,Pangjiahe,--,--,,,,,,,,,,,
102,Pegao,Same as RE00789,on Laizishan short axial anticline,,,,,,,,,,,
103,Peyian,Same as RE00789,Same as RE00789,,,,,,,,,,,
104,Pingding,west Qinling transform zone,"north wing of Bailongjiang multiple anticline, which belongs to a sub-zone of western Qinling fold system. Deposit occurs in Jiuyuan-Pingding syncline",,,,,,,,,,,
105,Pingshan,--,--,,,,,,,,,,,
106,Pingtang,--,--,,,,,,,,,,,
107,Pingwang,--,--,,,,,,,,,,,
108,Posang,--,--,,,,,,,,,,,
109,Pulongba,--,--,,,,,,,,,,,
110,Puzilong,Same as RE00789,controlled by Huijiapu anticline which trend east to west,,,,,,,,,,,
111,Qiaoqiaoshang,west margin of Yangtze craton,Xueshan gold belt is composed of carbonate formation,,,,,,,,,,,
112,Qilicun,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
113,Qilixia,west Qinling transform zone,a series of folds and faults which trend east-west,,,,,,,,,,,
114,Qingkeyan,western Qinling transform zone,Bailongjiang gold belt is about 160 ~ 200 km long and trends east to west. It is distributed along with Bailongjiang thrust zone. Gold mineralization occurs in a black formations of Cambrian and Devonian,,,,,,,,,,,
115,Qingping,Same as RE00789,on north of Laizishan short axial anticline,,,,,,,,,,,
116,Qiuling,west Qinling transform zone,a series of folds and faults which trend east-west,,,,,,,,,,,
117,Qiuluo,--,--,,,,,,,,,,,
118,Quluopunongba,west margin of Yangtze craton,Ganzi-Xianshuihe gold belt trending northwest,,,,,,,,,,,
119,Quongmo,western Qinling transform zone,Bailongjiang gold belt is about 160 ~ 200 km long and trends east to west. It is distributed along with Bailongjiang thrust zone. Gold mineralization occurs in a black formations of Cambrian and Devonian,,,,,,,,,,,
120,Sanchahe,near buried southwestern margin of Precambrian Yangtze craton,deposit located along crest of 40 km long NW-trending anticline that exposes Permian strata in center,,,,,,,,,,,
121,Sanhua,--,--,,,,,,,,,,,
122,Sanrengou,western Qinling transform zone,near Liba gold deposit,,,,,,,,,,,
123,Shangshi,--,--,,,,,,,,,,,
124,Shaziling,Same as RE00789,Same as RE00789,,,,,,,,,,,
125,Shewushan,--,--,,,,,,,,,,,
126,Shijiba,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
127,Shixia,--,--,,,,,,,,,,,
128,Shuangwang,west Qinling transform zone,"Fengxian-Zhenan suborder fold in late Mesozoic age include Yuanbazi multiple syncline, Xiba multiple anticline and Xinghuongpu-Sangba multiple syncline. The breccia zone, which hosted deposit, is located at north wing of Xiba multiple syncline",,,,,,,,,,,
129,Shuiniujia,--,--,,,,,,,,,,,
130,Shuishengou,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
131,Sixiangchang,southwest margin of Yangtze craton,Sandu-Danzhai gold belt trending north to south,,,,,,,,,,,
132,Songpan,--,--,,,,,,,,,,,
133,Tangshang,Same as RE00789,Same as RE00789,,,,,,,,,,,
134,Tangxinzhai,Same as RE00789,on north of Laizishan short axial anticline,,,,,,,,,,,
135,Tianwan,--,--,,,,,,,,,,,
136,Tuanjie,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
186,Tuongkangling,"intersection of Tanlu rift and Huaiyang folds, Yangtze craton",tight close folds trending east-west were cut by igneous intrusion,,,,,,,,,,,
137,Wangmo,Same as RE00789,Same as RE00789,,,,,,,,,,,
138,Weihuai,Same as RE00789,at southeast of Laizishan short axial anticline,,,,,,,,,,,
187,Woxi,margin of Yangtze craton,"located in Proterozoic and Sinian silty argillite, sericite slate and siltstone",,,,,,,,,,,
139,Wuhan,--,--,,,,,,,,,,,
140,Xiangzicha,--,--,,,,,,,,,,,
141,Xiaojiapu,--,--,,,,,,,,,,,
142,Xichong,--,--,,,,,,,,,,,
143,Xidayu,--,--,,,,,,,,,,,
144,Xinguan,--,--,,,,,,,,,,,
145,Xinqiao,--,--,,,,,,,,,,,
146,Xongwu,Same as RE00789,Same as RE00789,,,,,,,,,,,
188,Yaerma,western Qinling transform zone,Bailongjiang gold belt is about 160 ~ 200 km long and trends east to west. It is distributed along with Bailongjiang thrust zone. Gold mineralization occurs in a black formations of Cambrian and Devonian,,,,,,,,,,,
147,Yangjishan,"intersection of Tanlu rift and Huaiyang folds, Yangtze craton",tight close folds trending east-west were cut by igneous intrusion,,,,,,,,,,,
148,Yangyou,Same as RE00789,on Laizishan short axial anticline,,,,,,,,,,,
149,Yaojian,west Qinling transform zone,a series of folds and faults which trend east-west,,,,,,,,,,,
150,Yata,near buried southwestern margin of Precambrian Yangtze craton,"gentile to locally moderately tight folds, sometime with high-angle faults, trend generally east-west",,,,,,,,,,,
151,Yiaxiang,western Qinling transform zone,Bailongjiang gold belt is about 160 ~ 200 km long and trends east to west. It is distributed along with Bailongjiang thrust zone. Gold mineralization occurs in black formations of Cambrian and Devonian,,,,,,,,,,,
152,Yichang,--,--,,,,,,,,,,,
153,Yingchanggou,--,--,,,,,,,,,,,
189,Zacuen,--,--,,,,,,,,,,,
190,Zaorendao,--,--,,,,,,,,,,,
154,Zhanghai,"intersection of Tanlu rift and Huaiyang folds, Yangtze craton",tight close folds trending east-west were cut by igneous intrusion,,,,,,,,,,,
155,Zheboshan,north margin of Yangtze craton,"Minjiang gold belt, 120 to 140 km long and trending north to south, is composed of a series of thrusts",,,,,,,,,,,
156,Zhen'an,--,--,,,,,,,,,,,
157,Zheyi,Same as RE00789,Same as RE00789,,,,,,,,,,,
158,Zhongqu,--,--,,,,,,,,,,,
191,Zhuongqu,western Qinling transform zone,"Nanping-Maqu gold belt, trending northwest and 200 km long, consists of three suborder thrust zones. Its major body is Baxi multiple-syncline which is made up of Triassic clastic and carbonate rocks.",,,,,,,,,,,
192,Zhutong,--,--,,,,,,,,,,,
159,Zimudang,southwest margin of Yangtze craton & Huanan fold system,"by influence and control from late Mesozoic tectonic activity, Faults and folds in this area trend as northeast, northwest and east-west. They overlapped or intersected each other so that more short-axial anticlines were developed on craton area, while mo",,,,,,,,,,,