摘要
Tertiary Junggar Basin has been subjected to a shrinking period.Affected by the Yanshan orogeny, especially the Himalayan movement,the Tianshan Mountain continued to rise,leading the southern margin to the sedimentary environment with steep slope and speed deposition.The major depositional facies in Ziniquanzi Formation is generally a set of delta under the setting of lake transgression,belonging to single deposi-
出处
《地学前缘》
EI
CAS
CSCD
北大核心
2009年第S1期139-140,共2页
Earth Science Frontiers