A test of different factors influencing the isotopic signal of planktonic foraminifera in surface sediments from the northern South China Sea

2005 ◽  
Vol 55 (1-2) ◽  
pp. 49-62 ◽  
Author(s):  
Ludvig Löwemark ◽  
Wei-Li Hong ◽  
Tzen-Fu Yui ◽  
Gwo-Wei Hung
Geosciences ◽  
2020 ◽  
Vol 11 (1) ◽  
pp. 8
Author(s):  
Mei Zhang ◽  
Hongfeng Lu ◽  
Qing Chen ◽  
Gayan Bandara ◽  
Hui Zhang ◽  
...  

In the northern South China Sea, pockmarks are widely distributed on the seabed offshore on the southwestern Xisha Uplift. The mineralogy and geochemistry of the clay minerals and surface sediments from the pockmark field were identified using X-ray diffraction (XRD) analysis and X-ray fluorescence (XRF) analysis to trace the provenance, weathering, and sediment transportation system in the area. The clay minerals are primarily comprised of illite, smectite, kaolinite, and chlorite, showing a distribution of average weight percentages of 35%, 35%, 18%, and 13%, respectively. Based on the surrounding fluvial drainage basins and various transport mechanisms (current or monsoon), illite and chlorite primarily originate from rivers in Taiwan and the Mekong and Red Rivers. Kaolinite primarily originates from the Pearl River, and smectite derived from the Luzon arc system is primarily transported by surface currents with significant influence from the Kuroshio intrusion.


2013 ◽  
Vol 4 (2) ◽  
pp. 223-229 ◽  
Author(s):  
Huangmin Ge ◽  
Chuanlun L. Zhang ◽  
Hongyue Dang ◽  
Chun Zhu ◽  
Guodong Jia

2014 ◽  
Vol 25 (1) ◽  
pp. 189-196 ◽  
Author(s):  
Weihai Xu ◽  
Wen Yan ◽  
Zhong Chen ◽  
Han Chen ◽  
Weixia Huang ◽  
...  

Palaeoworld ◽  
2020 ◽  
Vol 29 (3) ◽  
pp. 636-647 ◽  
Author(s):  
Ismail Adejare Ladigbolu ◽  
Bao-Hua Li ◽  
Hong-Liang Li ◽  
Martin G. Wiesner ◽  
Zhou-Fei Yu ◽  
...  

Sign in / Sign up

Export Citation Format

Share Document