STRUCTURE TYPE AND FORMATIVE MECHANISM OF WEST SHANDONG COALFIELD
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Graphical Abstract
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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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