2016
DOI: 10.1007/s12517-016-2674-5
|View full text |Cite
|
Sign up to set email alerts
|

Fine-grained and coarse-grained Paleogene sublacustrine fan systems in Fushan Depression, Beibuwan Basin, South China Sea: implications for sedimentary characteristics and depositional processes

Abstract: The Fushan Depression is a hydrocarbon-bearing half-graben rift sub-basin located in the southeast of the Beibuwan Basin, South China Sea. The sublacustrine fan systems in the Paleogene Liushagang Formation have recently become important targets in this depression, while the depositional process and detailed characterization of these systems are little known. Analysis of drilled cores, wire-line logs, and 3-D seismic survey suggest that the Fushan Depression develops two different types of sublacustrine fan sy… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

2019
2019
2020
2020

Publication Types

Select...
2

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(2 citation statements)
references
References 29 publications
0
2
0
Order By: Relevance
“…In the Qiongdongnan Basin, the littoral to lacustrine facies mainly dominated the NE‐trending central depressions, while fluvial–alluvial fan and relevant submarine fan facies were limited to areas near Hainan Island in the northwestern part of the basin. Similarly, a dominance of littoral to lacustrine facies and partly fluvial, deltaic and fan facies were also developed in the Beibuwan Basin and the Phu Khanh Basin (Fyhn, Boldreel, & Nielsen, ; Pan et al, ; J. Wang, Cao, & Li, ).…”
Section: Cretaceous–early Oligocene Sedimentary Evolutionmentioning
confidence: 94%
See 1 more Smart Citation
“…In the Qiongdongnan Basin, the littoral to lacustrine facies mainly dominated the NE‐trending central depressions, while fluvial–alluvial fan and relevant submarine fan facies were limited to areas near Hainan Island in the northwestern part of the basin. Similarly, a dominance of littoral to lacustrine facies and partly fluvial, deltaic and fan facies were also developed in the Beibuwan Basin and the Phu Khanh Basin (Fyhn, Boldreel, & Nielsen, ; Pan et al, ; J. Wang, Cao, & Li, ).…”
Section: Cretaceous–early Oligocene Sedimentary Evolutionmentioning
confidence: 94%
“…Compared to the limited Palaeocene records, the Eocene syn-rift sediments are widely distributed on the South China Sea conjugate margins (Figure 9). In the Taiwan region, the Lower-Middle Eocene (Fyhn, Boldreel, & Nielsen, 2009;Pan et al, 2016;J. Wang, Cao, & Li, 2012).…”
Section: Early-middle Eocenementioning
confidence: 99%