首页 | 本学科首页   官方微博 | 高级检索  
     检索      

FORMATION OF GOLD-BEARING HYDROFRACTURING BRECCIA BODIES IN TECTONIC LENSES: A CASE STUDY ON SHUANGWANG GOLD DEPOSIT, SHAANXI, CHINA
作者姓名:ZENG  Qiaosong  WANG  Jincao  CHEN  Guanghao
作者单位:[1]Key Laboratory of Mineralization Dynamics, Chinese Academy of Sciences, Guangzhou, Guangdong 510640, China; [2]Dept. of Resources and Environmental Engineering, Guilin Institute of Technology,Guilin, Guangxi 540014, China [3]School of Graduate Study, Chinese Academy of Sciences; Beijing 100083, China
基金项目:国家"305"科技攻关项目,the Key Innovation Oriented Program
摘    要:1 Introduction Hydrofracturing is possibly an important fracture behavior within the whole lithospheric crust, many geologists have noticed and carried out study on hydrofracturing in the fluid-rock systems (e.g., Phillips, 1972; Sibson, 1986; Fyfe, 1987; Svyatoslav and Kirill, 1993; Cox, 1995; Nakashima and Toriumi, 1996; James et al., 2000; Agust et al., 2002). Hydrofracturing phenomena are universally existent in the active structural belts, nonlinear tension vein systems in metamorphi…

关 键 词:水力压裂  角砾岩  沉淀物  秦岭  陕西
文章编号:1006-513X(2005)02-0093-14
收稿时间:2005-11-03
修稿时间:2005-11-20

FORMATION OF GOLD-BEARING HYDROFRACTURING BRECCIA BODIES IN TECTONIC LENSES: A CASE STUDY ON SHUANGWANG GOLD DEPOSIT, SHAANXI, CHINA
ZENG Qiaosong WANG Jincao CHEN Guanghao.FORMATION OF GOLD-BEARING HYDROFRACTURING BRECCIA BODIES IN TECTONIC LENSES: A CASE STUDY ON SHUANGWANG GOLD DEPOSIT, SHAANXI, CHINA[J].Geotectonicaet Metallogenia,2005,29(2):93-106.
Authors:ZENG Qiaosong  WANG Jincao  CHEN Guanghao
Abstract:Macro-microscopic tectonic analysis and lithologic features show that the gold-bearing breccia bodies in the Shuangwang gold deposit, for hydrofracturing of the deep-sourced and alkali-rich fluids in the Devonian sodic rock series, are identified as hydrofracturing breccia bodies. Since the Indosinian,intracontinental collisional orogenesis results in multiple fracturings and magmatic emplacements in the Qinling area. Deep-sourced fluids resulting from deep fractures and granitoid magmatic intrusion are of a supercritical nature. Joint action between the fluid-rock system and structures leads to hydroffacturing and ore formation of the gold deposit.Firstly, the progressive coaxial compression caused the competent sodic rock series and the incompetent pelitic rock series to be deformed and partitioned. Lens-like weak-strain domains are hence formed and distributed at the approximate equidistance zones and the linear strong-strain zones,respectively. Subsequently, the progressive non-coaxial shearing and right-lateral and high-angle oblique thrusting lead to the most developed fracture system in the core of the weak-strain domain to turn from compression to extension and to link up with the deep fracture systems. The periodical huge pressure decline in the pumping center causes the deep-sourced confined fluids to develop periodic tectonic pumping, hydrofracturing and precipitation-healing in the sodic rock series. The gold-bearing hydrofracturing breccia bodies are hence ultimately formed at near-equidistance tectonic lenses. On the basis of the above model, the predicted concealed gold-bearing hydrofracturing breccia bodies have been preliminarily validated by latest drillings.
Keywords:hydrofracturing  sodic breccia  deformation and partitioning  Shuangwang gold deposit  Qinling
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号