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《Geology of Anhui》 2000-04
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THE DISCOVERY OF PYROCLASTIC ROCKS IN THE ZHOUGONGSHAN FORMATION OF XIAOHUASHAN,LU’ AN AND THE STRATIGRAPHIC IMPLICATIONS

WANG Dao- xuan,LI Shuang- ying,LIU Yin,JIN Fu- quan (Department of Resources and Environmental Sciences,Hefei University of Technology,Hefei 230009,China)  
Sedimentary pyroclastic rocks are discovered in the red sandstones of the Zhougongshan Formation,Xiaohuashan, Lu` an city, Auhui. Lithologically they belong to andesitic tuffaceous bressia and tuffite or tuffaceous sandstones. There are a variety of forms of gravels(debris),less of them take the form of flame or thin sheet as a product simultaneous with eruption. It has been shown by microscopic study that the debris of volcanics is fresh and the lithologic features are exactly like those of the upper Jurassic Maotan chang Formation in the erosion source area. So the Zhougongshan Formation is thought to be diachronous,ranging from the Maotanchang stage to Heishidu stage,with its main part equivalent to the latter. It is a heteropic product synchronous with the Heishidu Formation and deposited in the early Cretaceous.
【Fund】: 中科院 KE951- A1- 401- 07项目
【CateGory Index】: P588.2
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