Very high resolution seismic record were used to study the sedimentary processes and morphosedimentary features of the continental slope system since Miocene in Qiongdongnan Basin(QDNB),offshore Hainan,northern South ...Very high resolution seismic record were used to study the sedimentary processes and morphosedimentary features of the continental slope system since Miocene in Qiongdongnan Basin(QDNB),offshore Hainan,northern South China Sea.It can be divided into four types based on the sedimentary processes and morphology:wide and gentle slope,sigmoid-progradational slope,slumping slope and channeled slope.Different features of展开更多
The Qiongdongnan Basin lies in the west part of the northern South China Sea.To the west the basin is bound by the Red River Fault and the Yinggehai Basin,to the east by the Pearl River Mouth Basin,and to the south by...The Qiongdongnan Basin lies in the west part of the northern South China Sea.To the west the basin is bound by the Red River Fault and the Yinggehai Basin,to the east by the Pearl River Mouth Basin,and to the south by the Xisha Rise.In this study,the sequence stratigraphic framework was set up and 11 third-order sequences were distinguished.Based展开更多
文摘Very high resolution seismic record were used to study the sedimentary processes and morphosedimentary features of the continental slope system since Miocene in Qiongdongnan Basin(QDNB),offshore Hainan,northern South China Sea.It can be divided into four types based on the sedimentary processes and morphology:wide and gentle slope,sigmoid-progradational slope,slumping slope and channeled slope.Different features of
文摘The Qiongdongnan Basin lies in the west part of the northern South China Sea.To the west the basin is bound by the Red River Fault and the Yinggehai Basin,to the east by the Pearl River Mouth Basin,and to the south by the Xisha Rise.In this study,the sequence stratigraphic framework was set up and 11 third-order sequences were distinguished.Based
