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《Acta Geologica Sichuan》 2011-01
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Where from the Earthquake Stone

QIAO Bao-cheng LI Yong YAN Liang WANG Jin-cheng(State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059)  
There is an earthquake stone in the earthquake vestige park in Donghekou,Qingchuan.The study indicates that the so-called earthquake stone is an altered diabase-porphyrite which was formed in Hercynian-Indochinese epoch and subjected late alteration.It was transported to present location by the Wangjiashan Landslide during the Wenchuan Earthquake.
【Fund】: 国家自然科学基金项目(40972083)
【CateGory Index】: P315.2
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