松辽盆地东缘下白垩统营城组二段火山碎屑岩的发育特征

通过精细的野外剖面测量，发现松辽盆地东缘营城组二段中发育熔岩、凝灰岩和凝灰质砂岩。凝灰岩包括熔结凝灰岩、岩屑晶屑凝灰岩、灰球泥粒凝灰岩和角砾凝灰岩。这表明作为火山活动间歇期的营城组二段沉积期依然存在一定规模的火山活动，其沉积作用具有独特的火山和沉积双重控制的特点，区别于正常的沉积作用。营城组二段是一套介于火山岩和陆源碎屑岩之间的过渡岩性，物源既有来自同期火山喷发，也有来自营城组一段和营城组下段以及更老的地层的风化剥蚀。由于存在火山物质和陆源剥蚀物质的双重物源及存在火山物质堆积和沉积作用的双重机理，这套岩石在类型上具有特殊性。存在特殊的火山-沉积作用类型，主要为冲积平原上热碎屑流河道沉积、冲积平原泛滥盆地上热基浪沉积、冲积平原泛滥盆地上空落火山灰云沉积。

Characteristics of Volcaniclasitic Rocks Developed in Member 2,Yingcheng Formation,Lower Cretaceous,in the Eastern Margin of Songliao Basin

The volcanic lava,tuff and tuffaceous sandstones were recognised in member 2 of Yingcheng Formation,Cretaceous in the survey of outcropped geological section with a detailed measurement in the eastern margin of Songliao basin.The tuff rocks include ignimbrite,lithic crystal tuff,ash ball tuff and breccia tuff.It indicates that a certain scale of volcanic activities still existed during the forming of member 2 of Yingcheng formation,which was a stage without strong volcanic activities.This kind of deposition...