Block faulting tectonics, as the dominant tectonic framework of western Shandong, were formed by the extensional linked fault system through two extensional movements during the Mezo-Cenozoic. The two extensional movements had the same evolutional process
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燕守勋.1996.鲁西地壳隆升的伸展构造模式[J].地质学报,70(1). Yan Shouxun,.1996. EXTENSIONAL TECTONIC MODEL OF CRUSTAL ELEVATION IN WESTERN SHANDONG[J]. Acta Geologica Sinica,70(1).