| PDF: | |
| Time: | 2003 |
| Journal: | Oil & Gas Geology |
| Volumn: | 24 |
| Issue: | 1 |
| Pages: | 24-27 |
| Type: | Other |
| Author: | Rihui Cheng,Wanzhu Liu,Pujun Wang,Xuanlong Shan,Shumin Chen,Yongbao Qu. |
Abstract: | The volcanic rocks in Xujiaweizi fault-depression , Songliao basin ,was mainly erupted in Late Jurassic to Early Cretaceous.Their occurences are characterized by a certain geometric pattern.On the basis of the structural position of volcanic eruption and the occurrences in the basin, three types of eruption have been identified , including eruption on the upthrown side of fault, along fracture belt and on downthrown side.Different occurrences are often corresponding to different basin structures.The volcanic rocks occurring along fault plane would transit gradually to sublacustrine fan—turbidite fan;the volcanic rocks occurring on the upthrown side of fault would distribute in the manner of alternating beds of volcanic rocks and sandstones;the volcanic rocks occurring on the downthrown side have mostly been covered by fine grain sediments. |