Abstract
The control of synchronous structures on formation of superlarge stratabound ore deposits is immense. Based on studies of ore deposits in South Qiniing, northern Guangdong, Langshan and other areas, three new ideas in comparison with examples of ore control of synchronous structures both in China and abroad are proposed: (i) multiorder ore control of synchronous structures, which means that synchronous structures of different orders display different controls on ore deposits; (ii) synchronous structures in different stages of basin evolution display different controls on basin fluid system and ore-forming system; (iii) synchronous strurture accompanying hydrothermal mineralization as a preexisting weak surface in earth crust often reactivate in later tcctono-thermal event to be a channelway for magma or thermal fluids which superimposed on and reformed preexisting ore beds to form large or superlarge composite ore deposits.
Similar content being viewed by others
References
Tu, G. Z., Recent progresses in the studies and researches for superlarge mineral deposits,Earth Science Frontiers (in Chinese). 1994, (1): 45–52.
Cheng, X. J., Ore control of synsedimentary fault,Mineral Deposits (in Chinese), 1994 (special issue): 110
Zhai, Y. S., Zhang, H., Song, H. L.,Macroscopic Structure and Superlarge Ore Deposits (in Chinese), Beijing: Geological Publishing House, 1997, 51–92.
Geng, S. F., Yan, K. Z., Zhou, W. Q.,Metallogenic Regularities of Main Metallic Minerals in Qinling-Dabashan Mountains (in Chinese), Beijing: Geological Publishing House, 1994, 91–94.
Wang, J. L., He, B. X., Li, J. Z.,Qinling-type Lead-zinc Deposits in China (in Chinese), Beijing: Geological Publishing House, 1996, 264.
Lai, Y. Q., Genesis of Fankou Pb-Zn deposit,Geological Review (in Chinese), 1988, 34(3): 220–230.
Zhai, Y. S., Yao, S. Z., Lin, X. D.,Metallogeny of Iron and Copper (Gold) Deposits in the Middle-Lower Yangtze Region (in Chinese), Beijing: Geological Publishing House, 1992, 188–190.
Yue, W. Z., Ye, Z. Z., Wei, N. Y.,Sedimentary Geology and Stratabound Massive Sulphide Deposits of Late Carboniferous Weining Age in the Middle and Lower Yangtze Reaches (in Chinese), Beijing: Geological Publishing House, 1993, 126.
Zhai, Y. S., Deng, J., An outline of mineral resources of China and their tectonic setting,Australian Journal of Earth Sciences, 1996, (4): 673–685.
Xu, J., Synsedimentary structure and mineralization in Dachang tin-polymetallic deposit,Mineral Deposits (in Chinese), 1994 (special issue): 103.
Pang, Q. Y., Geological background and genesis of Baiyan Obo REE-Te deposit,North China Geology & Mineral Resources Journal (in Chinese), 1996, 11(3): 369.
Chen, X. M.,Tectonic Evolution, Deposit Model and Ore Predication, Beijing: Geological Publishing House, 1992.
Cheng, X. J., Zhai, Y. S., Basin synsedimentary fault and its control of stratabound Pb-Zn-(Ba-&-Ag) deposits,Beijing Geoscience—Journal of Graduate School, China University of Geosciences (in Chinese), 1995, (3): 343.
Maclntyre, D. G., SEDEX-sedimentary-exhalative deposit, inOre Deposits, Trctonics and Metallogeny in the Canadian Cordillera (eds. McMillan, W. J., Hoy, T.), Victoria: Queen’s Printer for British Columbia, 1995, 25–76.
Maclay, K. R., Deformation of stratiform Pb-Zn (-barite) deposits in the north Canadian Cordillera,Ore Geology Reviews, 1991, (6): 435.
Author information
Authors and Affiliations
Additional information
Project supportvd by the National Climbing Program of Chlna (A30).
Rights and permissions
About this article
Cite this article
Zhai, Y., Deng, J., Song, H. et al. Synchronous structure control of superlarge ore deposits. Sci. China Ser. D-Earth Sci. 41 (Suppl 1), 7–12 (1998). https://doi.org/10.1007/BF02875632
Received:
Issue Date:
DOI: https://doi.org/10.1007/BF02875632