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通化县四方山铁矿地质特征
引用本文:刘先权,高明珠,韩雪,车海龙,路猛,张庆连.通化县四方山铁矿地质特征[J].吉林地质,2014(3):50-55.
作者姓名:刘先权  高明珠  韩雪  车海龙  路猛  张庆连
作者单位:1. 通化县四方山铁矿,吉林通化,134107
2. 吉林省第四地质调查所,吉林通化,134001
3. 吉林星泰集团有限公司,吉林白山,134300
摘    要:四方山铁矿经历了三期变形。第一期,当太古宙表壳岩形成后,来自东西向挤压作用,地层和矿体(S0)形成近南北向紧密褶皱构造。第二期,来自北西—南东方向挤压作用,使已经变形地层和矿体(S1)又一次变形,形成走向北东—南西叠加褶皱构造,这一期为四方山铁矿主期构造。第三期,来自北—西向和南东向不对称推力作用,使已经历二次变形地层、矿层均形成了S形,使S2又一次变形。

关 键 词:四方山铁矿  表壳岩  变质变形  背斜  向斜  叠加褶皱

Geological characteristics of Sifangshan iron ore in Tonghua County
LIU Xian-quan,GAO Ming-zhu,HAN Xue,CHE Hai-long,LU Meng,ZHANG Qing-lian.Geological characteristics of Sifangshan iron ore in Tonghua County[J].Jilin Geology,2014(3):50-55.
Authors:LIU Xian-quan  GAO Ming-zhu  HAN Xue  CHE Hai-long  LU Meng  ZHANG Qing-lian
Institution:LIU Xian-quan, GAO Ming-zhu, HAN Xue, CHE Hai-long, LU Meng, ZHANG Qing-lian( 1. Sifangshan iron ore of Tonghua County, Tonghua 134107, Jilin, China;2. The Fourth Geological survey of Jilin Province, Tonghua 134001 Jilin, China ; 3.Jilin Xingtai Group Co. Ltd, Baishan 134300, Jilin, China)
Abstract:Sifangshan iron ore had experienced three phases of deformation. The first period, the strata and ore bodies (S0) occurred near South-North tight folds by pressed from E-W extrusion effect, after the formation of Archean supracrustal rocks, The second stage, deformed the strata and ore bodies(S1) were deformed again , from the North West-South East direction compression, this period was Sifangshan iron main structure. The third stage , the strata and ore bodies which had experienced twice deformation formed an S shape, due to the asymmetric thrust from the North-West and South East direction , so that S2 deformed. once again.
Keywords:Sifangshan iron  supracrustal rocks  metamorphism and deformation  anticline syncline  superimposed folds
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