摘要
江西修水县西北部下志留统梨树窝组第１、２段为一套较深水的浊积岩，可划分为６个浊积岩相，能组合成６个浊积岩相组合，自下而上反映了一种向上变粗、变厚的推进型浊积扇序列，
deep turbidite is discovered in the lower part of Lishuwo Forma-tion of the Lower Silurian in northwest Xiushui County,Jiangxi Pro-vince,and can be divided into six turbidite facies which constitute sixtusbidite facies assemblages.By facies analysis,a prograding turbidite fan sequence has beenestablished
出处
《江西地质》
1995年第1期37-44,共8页
Jiangxi Geology
