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《REGIONAL GEOLOGY OF CHINA》 1999-02
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Discovery and geological characteristics of rhyolitic vitroclastic rocks in Northern Hebei

XIA Guo li (Institute of Regional Geological Survey, Hebei Bureau of Geology and Mineral Exploration and Development, Langfang, Hebei 065000,China)  
Tumulose rhyolitic vitroclastic rocks were first found in the Beiliang volcanic edifice. They occur in a layer of acid volcanic rocks of the Late Jurassic Zhangjiakou Formation. The content of spheroids in such kind of rocks is more than 80%. They are generally 0.5~10 cm in diameter, and the cement is cryptocrystalline and glassy lavas. In the lower part of the layer the spheroids show the distinct rolling feature and a well developed layered structure; in the upper part the spheroids do not roll and have a parallel planar flow structure. The spheroids were formed by quenching and clastation of erupted volcanic agglomerates and breccias when wet and rounding of the resulting fragments during rolling.
【Key Words】: Beiliang volcanic edifice rhyolitic vitroclastic rocks Zhangjiakou Formation
【CateGory Index】: P588.211
【DOI】: CNKI:SUN:ZQYD.0.1999-02-002
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