王淑霞, 张凡斌, 滕祥雷, 胡今朝. 鲁西煤田构造类型及形成机制[J]. 华北地震科学, 2008, 26(3): 36-38.
引用本文: 王淑霞, 张凡斌, 滕祥雷, 胡今朝. 鲁西煤田构造类型及形成机制[J]. 华北地震科学, 2008, 26(3): 36-38.
WANG Shu-xia, ZHANG Fan-bin, TENG Xiang-lei, HU Jin-zhao. STRUCTURE TYPE AND FORMATIVE MECHANISM OF WEST SHANDONG COALFIELD[J]. North China Earthquake Sciences, 2008, 26(3): 36-38.
Citation: WANG Shu-xia, ZHANG Fan-bin, TENG Xiang-lei, HU Jin-zhao. STRUCTURE TYPE AND FORMATIVE MECHANISM OF WEST SHANDONG COALFIELD[J]. North China Earthquake Sciences, 2008, 26(3): 36-38.

鲁西煤田构造类型及形成机制

STRUCTURE TYPE AND FORMATIVE MECHANISM OF WEST SHANDONG COALFIELD

  • 摘要: 根据鲁西煤田断裂、褶曲构造的独特特征,分析了控煤构造的主要类型及形成机制,由于郯庐、聊考断裂长期左行平移,控制了鲁西煤田构造演化特征,形成了鲁中"掀斜式"断块构造和鲁西南"堑垒式"断块构造两种截然不同的构造格局,并对今后找煤工作的方向进行了初步的探讨。

     

    Abstract: Based on the special characteristics of faults and bending folds in West Shandong Coalfield, the main type and its formative mechnism of coal structure are analyzed.The longterm left translation of Liaokao and Tanlu fault controled the tectonic evolvement of Luxi Coalfield, and formed central Shandong oblique Block and southwest Shandong rift valley two different kind structures.

     

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