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31. The result of application in many goldfields has showed that structural superimposed halo is an effective method on gold exploration and prognosis in deep and periphery of gold deposit.

32. This is a preliminary summation of the geological features of the cataclastic albitite type gold deposit in Dagougu area, northern Guangdong Province.

33. Chaoshan gold deposit is located at the Shizishan ore-field in Tongling, Anhui Province and the host rock is the Baimangshan augite diorite.

34. Dahuabei granite genesis of Wulashan gold deposit belongs to the continental crust ( remould ) remelting type.

35. Dongfengshan gold deposit is occurred in hornstone of Dongfengshan group under iron bearing stratum.

36. Wunan gold deposit is located in the active zone of northern margin of Tarimu plate, which concretely exist in the structure unit of triphibian edge in the late Paleozoic in southern Tianshan.

37. A systematic study on the characteristics in distribution, chemical composition, crystal texture, crystal morphology and pyroelectricity of pyrite has been made in the Wulong gold deposit.

38. Shuijingtun gold deposit is located in the central axis of the Zhanjiakou-Xuanhua mantle branch and in the west of alkaline hornblende monzonite in the area of Shuiquangou-Dananshan in Zhangjiakou.

39. There is a close relationship of gold mineralization to silicification, sericitization and chloritization. The potential reserves of this deposit may exceed a large size gold deposit.

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40. Songshunangou gold deposit is located in the volcano - tectonic depression, the mineralization relates to volcanic rock.

41. The Mobin gold deposit is a. low-medium temperature, sulfide-poor and gold-bearing quartz vein deposit.

42. Xiangluwanzi gold deposit is a volcanogenic hydrothermal ore deposit related to volcanic cryptoexplosive breccia body.

43. Mawu deposit is a medium-scale gold deposit, located in the east part of Minxian and the middle of metallogenic belt Min-Li.

44. Nickel, cobalt and palladium electrodeposits used as barrier layer between copper basis and gold deposit can effectively reduce migration of copper atom to gold upper deposit.

45. Guilaizhuang gold deposit is an epithermal gold deposit of Te-Au type related to alkaline subvolcanic rocks and controlled by crypto-explosive breccias.

46. The Dongan gold deposit in Xunke county , Heilongjiang province, epithermal type gold deposit recently discovered.

47. The lateritical gold deposit is an lately-founded indiscernible and a new type of gold deposit.

48. The deposit is a typical meso - epithermal magmatic gold deposit related to continental sub - volcanism.

49. This discovery has practical significance for look for placer gold deposit in Guangxi.

50. The formation of the gold deposit had undergone the process of migmatization , ductile sheering and magmatic hydrothermal superimposition.

51. Calcareous siltstone is the main host rock of micro fine disseminated gold deposit(MDGD).

52. The most important country rock alterations are silicification, sericitization and pyritization which are closely associated with gold deposit.

53. The deep mineral potential of gold is evaluated by analyzing and testing the form, composition and thermoelectricity of pyrite in the Nanzhangjia gold deposit.

54. Sheweishan gold deposit is a large - scale laterite - type deposit first found in Hubei Province of China.

55. The controlling effect of the superimposition of two type folded structural systems on gold deposit provides guiding significance for determining ore prospect orientation.

56. The Aketishikan gold deposit is located in the east of southern Nurt area, north of Altay.

57. Ankerite is one of the main gangue minerals genetically related to gold mineralization in the Baguamiao giant gold deposit.

58. The Dongping super large gold deposit has close relation with the Shuiquangou alkalic complex.

59. The gold telluride deposit is an important type of gold deposit.

60. Ajialongwa deposit is an epithermal fine - disseminated gold deposit.