The late Cenozoic deep-water channel system in the Baiyun Sag, Pearl River Mouth Basin: Development and tectonic effects

2015 ◽  
Vol 122 ◽  
pp. 226-239 ◽  
Author(s):  
Benjun Ma ◽  
Shiguo Wu ◽  
Qiliang Sun ◽  
Lijun Mi ◽  
ZhenZhen Wang ◽  
...  
2013 ◽  
Vol 87 (1) ◽  
pp. 197-210 ◽  
Author(s):  
LI Yun ◽  
ZHENG Rongcai ◽  
YANG Baoquan ◽  
ZHU Guojin ◽  
GAO Boyu ◽  
...  

2013 ◽  
Vol 295-298 ◽  
pp. 2838-2841
Author(s):  
Ling Xiao ◽  
Han Wang ◽  
Qin Lian Wei

According to comprehensive researches on indicators of lithology,indicators of primary sedimentary structures,bioclasts and matrix, summarize sedimentary characteristics and origin for sandbody in the Zhujiang formation of the Well LW3-1-1. The main rock types are mid-coarse grained sandstone with heavy coloured mudstone at its top and bottom,followed by very coarse grained sandstone with fine gravel occurs locally. It is showed that the sandstones are well sorted with very low content of mud, and possess high compositional maturity and textural maturity. Massive bedding, typical inverse graded bedding and inverse-normal graded bedding occur in the sandstones. So in general, it is a set of sedimentation of grain flow and density-modified grain flow.


2015 ◽  
Vol 2 (1) ◽  
pp. 77-87 ◽  
Author(s):  
Gang Gao ◽  
Wenzhe Gang ◽  
Gongcheng Zhang ◽  
Wenjun He ◽  
Xin Cui ◽  
...  

2020 ◽  
Vol 190 ◽  
pp. 106945 ◽  
Author(s):  
Jian Fu ◽  
Cong Chen ◽  
Meijun Li ◽  
Zhongtao Zhang ◽  
Zulie Long ◽  
...  

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