The mechanisms of the infill textures and its implications for the five-floor zonation at the Dajishan vein-type tungsten deposit, China

作者: Xiangchong Liu , Huilin Xing , Dehui Zhang

DOI: 10.1016/J.OREGEOREV.2014.10.011

关键词:

摘要: Abstract Infill textures in thick veins are one of the most important characteristics vein-type tungsten deposits, China. One prerequisites for forming these is low wallrock permeability, but its mechanisms have not been well understood. In this contribution, we investigated leading to permeability at Dajishan deposit by conducting finite element computer experiments. The numerical experiments suggest that hydrostatic compression exerted high-pressure fluids on decreases significantly a short geological time. deeper part more likely create and form infill than shallower part. also prohibits fluid flow from fracture zone country rock limits water–rock interactions. Therefore, facilitates both focusing high ore-formation efficiency zones. These conclusions help us better understand five-floor zonation Dajishan.

参考文章(63)
Alison Ord, Bruce E. Hobbs, Chongbin Zhao, Convective and Advective Heat Transfer in Geological Systems ,(2008)
Xinmin Zhou, Tao Sun, Weizhou Shen, Liangshu Shu, Yaoling Niu, Petrogenesis of Mesozoic granitoids and volcanic rocks in south China : a response to tectonic evolution. Episodes. ,vol. 29, pp. 26- 33 ,(2006) , 10.18814/EPIIUGS/2006/V29I1/004
Mao Jingwen, Cheng Yanbo, Chen Maohong, Franco Pirajno, Major types and time–space distribution of Mesozoic ore deposits in South China and their geodynamic settings Mineralium Deposita. ,vol. 48, pp. 267- 294 ,(2013) , 10.1007/S00126-012-0446-Z
Christian David, Teng-Fong Wong, Wenlu Zhu, Jiaxiang Zhang, Laboratory measurement of compaction-induced permeability change in porous rocks: Implications for the generation and maintenance of pore pressure excess in the crust Pure and Applied Geophysics. ,vol. 143, pp. 425- 456 ,(1994) , 10.1007/BF00874337
S. E. Ingebritsen, M. S. Appold, The physical hydrogeology of ore deposits Economic Geology. ,vol. 107, pp. 559- 584 ,(2012) , 10.2113/ECONGEO.107.4.559