Acta Scientiarum Naturalium Universitatis Pekinensis

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A Research for Emplacement Mechanism and Structure of Yuanshishan Granitoid

DENG Jixin1, LIU Ruixun1, SHI Ge1, LIANG Jincheng2, FENG Zuohai2   

  1. 1School of Earth and Space Sciences, Peking University, Beijing, 100871; 2GuiLin Institute of Technology, GuiLin, 541004
  • Received:2001-03-27 Online:2002-03-20 Published:2002-03-20

广西圆石山花岗岩体构造与侵位机制初探

邓继新1, 刘瑞珣1, 史謌1, 梁金城2, 冯佐海2   

  1. 1北京大学地球与空间科学学院,北京,100871; 2桂林工学院资环系,桂林,541004

Abstract: Based on the analysis of thermal contact metamorphic aureoles, granitoid interior structure, quartz axis fabric and strain characters in the different rock unites of Yuanshishan granitoid and its wall rocks, the emplacement mechanism of Yanshishan granitoid was studied. The magmatic explictite dynamic was advanced in light of regional stress and magma dynamic research. Those conclusion was synthesized to ascertain the emplacement mechanism-granitic magma ascended in dikes with the minimum critical width of the magma ascending channels about 2.21~3.88m and located in the core of Yindianshan dome with the passive style of dyke explictite; the later unite is a kind of multiple emplacement mechanism with the character of active emplacement of ballooning.

Key words: emplacement mechanism, strain analysis, magmatic explictite, Yuanshishan

摘要: 在对圆石山岩体围岩热变质带及岩体内部构造研究的基础上,认识岩浆在上升、侵位过程中对围岩的作用及岩体各单元间在先后定位过程中的相互作用,从而确定岩体的侵位机制。同时运用岩浆动力学原理从另一个角度探讨其侵位驱动力。综上指出:经分凝后的活动性岩浆在深部侧向挤压和浮力的联合驱动下,沿深大断裂以最小临界宽度为2.21~3.88m的裂隙脉动上侵,整体以岩墙扩展的方式被动定位于银殿山穹窿的核部,但后期屋面前单元具有主动侵位的特点应为一种复合定位机制。

关键词: 侵位机制, 应变分析, 岩浆动力学, 圆石山

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