Volume 39 Issue 2
Feb.  2014
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Shen Yanjie, Cheng Rihui, Yu Zhenfeng, Xia Zhiwei, Zhang Zhen, 2014. Reworked Pyroclastics Deposits and Facies Model of Cretaceous Yingcheng Formation in Songliao Basin, NE China. Earth Science, 39(2): 187-198. doi: 10.3799/dqkx.2014.018
Citation: Shen Yanjie, Cheng Rihui, Yu Zhenfeng, Xia Zhiwei, Zhang Zhen, 2014. Reworked Pyroclastics Deposits and Facies Model of Cretaceous Yingcheng Formation in Songliao Basin, NE China. Earth Science, 39(2): 187-198. doi: 10.3799/dqkx.2014.018

Reworked Pyroclastics Deposits and Facies Model of Cretaceous Yingcheng Formation in Songliao Basin, NE China

doi: 10.3799/dqkx.2014.018
  • Received Date: 2012-03-28
  • Publish Date: 2014-02-01
  • The pyroclastics grain size characteristics, the pyroclastics composition and the pyroclastics rocks facies of two types of pyroclastics rocks samples of Yingcheng Formation in the southeast edge of Songliao basin, tuffs and tuffaceous sandstone, had been studied. The results show that, the pyroclastics had been transported at the beginning by volcanism excitation, however, traction flow, gravity flow and the double mechanism of traction flow and gravity flow controlled the transportation process. The conclusion drawn from pyroclastic microscopic characteristics study, genetic type analysis and lithofacies analysis of those samples in study area calculates that, the majority volcanic debris accumulation was composed of hot base surge and pyroclastic flow deposition and a small portion had been composed of fallout. The characteristics of detrital composition were those, there were a large amount of crystal fragments, a small amount of shard and lithic fragments, and the lithic fragments existed only in coarse grain composition. Studies suggest that, the pyroclastics outcropped in this area were the reworked pyroclastics in the depositional environment. There were 4 types of pyroclastics facies, the hot base surge in the previous valley, the pyroclastics flow in the previous valley and the base surge and fallout on the alluvial plain had been distinguished in this area. Based on the member Ⅱ of Yingcheng Formation in the southeast edge of Songliao basin, facies models of the reworked pyroclastics in these fluvial-alluvial plain sedimentary environments were established.

     

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