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61. Measurements of pyroelectricity of pyrite demonstrate that the mineralizing temperature of the gold deposit is low-moderate.

62. Wangjiawaizi gold deposit occurs in Lower Proterozoic opimetamorphic rock series.

63. Maoduqing gold deposit occurred in the green schist and marble stratum belt of paleoprotozoic Inner Mongolia.

64. The pyroelectricity characteristics of pyrite can be used as the indicators for prospecting of gold deposit.

65. Aikinite in the Qiyugou gold deposit, Henan Province has been studied by means of reflecting microscope, MPV-1 Type microphotometer, JCXA-733 Type electron microprobe and X-ray powder analysis.

66. Gravel cemented geological body, called solid formation, has been found in the fluvial sediment of Quaternary system in the exploration and mining of alluvial gold deposit in recent years.

67. The Baguamiao gold deposit in a sort of mesothermal hypothermal carbonate type gold deposit.

68. Longsheng shear zone type gold deposit is divided into quartz vein type[http://sentencedict.com/gold deposit.html], fine quartz vein type and quartz stockwork type deposit.

69. The gold deposit in Yangshan, Gansu Province, has at least 160 tons in proven reserve, Xiong Bilin, deputy director of National Development and Reform Commission's industry department, said yesterday.

70. Gold deposit is the top mineralize by now. the parichnos of hot water is next main works.

71. The gold deposit in metamorphic rocks of Liaohe Group of the Early Prole rozoic in southern Liaoning was considered as meta-hydrothermal one.

72. This gold deposit is located on the west of Huaxiongtai promontory and of Machaoying fracture zone.

73. Under favorable conditions, sellaite - fluorite type gold deposit will be formed from the solution.

74. This paper has analysed the Hunan alluvial gold deposit and its present mining status.

75. Pyrites in Dianfang gold deposit of Proterozoic explosive breccia type are mainly gold - bearing minerals.

76. Xiazhangzi gold deposit is strictly controlled by structural fracture zone, and the wall rock alterations are mainly of K feldsparization, pyritization, silication and carbonation.

77. The deposit belongs to vadose hot brine-supergene genetic eluvial clay-type gold deposit and to laterite-type gold-deposit in terms of industry.

78. Gold deposit was prepared with a process of non-cyanide gold pulse electroplating in sulfite system, which is applicable to cavum target.

79. Silicification, potassic alteration, pyritization and sericitization are main alterations for the gold deposit.