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从褶曲到断层——构造形态认识的转变
引用本文:梁永平.从褶曲到断层——构造形态认识的转变[J].中国煤炭地质,2009(11):10-12.
作者姓名:梁永平
作者单位:宁夏回族自治区煤田地质局第一勘查院,宁夏银川750001
摘    要:王洼勘探区位于固原含煤区,勘探区整体为一走向近南北至北北西、向东倾伏的单斜构造,地层走向与构造的走向基本一致。在详查阶段确定区内发育王洼背斜、范新庄向斜。通过王洼扩大勘探后,根据新增钻孔资料分析,区内西南部发育一条走向NNE,倾向W的正断层(F7),倾角60°~80°,由南部延伸至勘探区,落差0-200m,尖灭于中北部的第4勘探线附近。据此认为原定的王洼背斜、范新庄向斜实为断层F7在断裂过程中所引起的牵引变形。

关 键 词:褶曲  断层  牵引变形  王洼勘探区

From Fold to Fault-the Concept Change on Structural Forms
Liang Yongping.From Fold to Fault-the Concept Change on Structural Forms[J].Coal Geology of China,2009(11):10-12.
Authors:Liang Yongping
Institution:Liang Yongping (The First Exploration Institute, Ningxia Bureau of Coal Geological Exploration, Yinchuan, Ningxia 750011)
Abstract:The Wangwa exploration area is located in the Guyuan coal-bearing zone, as a whole, the exploration area is a monoeline with near NS to NNW strike and plunging east, stratigraphic strike is basically identical with structural strike. The Wangwa anticline and the Fanxinzhuaug syncline have identified during preliminary exploration stage. Through extending exploration of Wangwa exploration area, based on newly drilled borehole data analysis, a normal fault (F7) with NNE strike, dipping west and dip angle 60°- 80°, throw 0-200m has found in southwestern exploration area, extending from south into the exploration area, pinch out near the No. 4 exploration line in middle north part. In view of the above, the paper concluded that the originally identified Wangwa anticline and Fanxinzhuang syneline are tractive deformations during the F7 fracturing process actually.
Keywords:fold  fault  tractive deformation  Wangwa exploration area
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