Abstract
Based on detailed geologic study, the important role of structuring in the formation of gold deposits in the area is discussed with special reference to structural evolution. Syngenetic faulting contemporaneous with tectonic-volcanic events is thought to be responsible for providing the ore-forming material at depth. The lithofacies formed by highly alternating deposition of terrestrial and carbonate detritus is chemically characterized by the assemblage of Au−Sb−As, constituting a favorable source bed for the activation and enrichment of gold. This gold source bed has undergone four major stages of structural deformation, accompanied by multi-staged alteration and mineralization.
Similar content being viewed by others
References
Item 321, IGCP, 1993, The Growth of Asia: Beijing, Earthquake Press, 95–98.
Kalbakova, N. N. and B. O. Manuchariats, 1990, Physicochemical condition of formation of antimony and gold-antimony mineralization: Geochemistry, n. 12, p. 1756–1765, (in Russian).
Wang Junfa, Zhang Fuxin, Yan Jincai, and Chen Ling, 1991, Strata-bound ore deposits in Devonian System, Qinling: Xi’an, Shaanxi Science and Technology Press, Xi’an, p. 47–48 (in Chinese).
Zhang Fuxin and Liu Wenfeng, 1992, Types and prospects of Devonian strata-bound gold deposits in Qinling: Journal of Northwest University (Natural Science Edition, supplement), p. 213–220 (in Chinese).
Zhang Fuxin, Liu Wenfeng, and Wei Kuangyi, 1993, Characteristics and evolution of gold-bearing pyrite in Jinlongshan-Qiuling gold deposit, Ding-Ma ore belt, Shaanxi, China: Geology and Prospecting, v. 29, p. 27–32 (in Chinese).
Author information
Authors and Affiliations
Additional information
This project was finantially supported by the Gold Head Quarters of the Chinese People’s Armed Forces and the Provincial Natural Science Foundation of Shaanxi, China.
Rights and permissions
About this article
Cite this article
Fuxin, Z., Jianqin, M. & Kuangyi, W. Formation of the micro-disseminated strata-bound gold deposits, with special reference to structural evolution, Miliang area, Zhen’an County, Shaanxi Province, China. Chin. J. of Geochem. 15, 314–323 (1996). https://doi.org/10.1007/BF02867005
Issue Date:
DOI: https://doi.org/10.1007/BF02867005