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High-resolution paleomagnetic records during 11.5-14.5 ka from the northern S...
The dataset contains the inclination and relative paleointensity (RPI) data during 11.5-14.5 ka of core NC2，which is located at the northen South China Sea (114.27E, 21.67N).... -
Relative intensity and age depostion range in the north of the South China Se...
Relative intensity (RPI) was constructed using the equation:RPI=NRM((20-60)mT)/SIRM (20-60)mTwhere SIRM were imparted with DC fields of 1000 mT, then demagnetized using 20,... -
Stacked dole effect in the north of the South China Sea from sediment core PC...
Relative intensity proxy (RPI) be constructed using the equation: RPI=NRM/SIRM (20-60)mT * MDFSIRM-CM/MDFSIRM, where MDFSIRM-CM is the center of mass of MDFSIRM -
Oxygen isotope and sea surface temperatue of the South China Sea from sedimen...
The oxygen isotope of was measured for the clean tests of Globigerinoides sacculifer planktonic foraminifera reacted with 100% orthophosphoric acid at 70 °C for 12 hours. Oxygen... -
Inclination of the South China Sea from sediment core PC27, PC83 and PC111
Normal remanent magnetization (NRM) and stepwise alternating field (AF) demagnetization were performed on the box samples with peak fields of 0-90 mT in 10-mT step and analysed... -
Dole effect in the north of the South China Sea from sediment core PC27 and PC83
Relative intensity proxy (RPI) be constructed using the equation: RPI=NRM/SIRM (20-60)mT * MDFSIRM-CM/MDFSIRM, where MDFSIRM-CM is the center of mass of MDFSIRM.Dole effect was... -
The relative paleointesnity and Dole effect in the north of the South China Sea
This dataset is including the relative paeleointensity (RPI), oxygen isotope, sea surface temperature and Dole effect data over the past ~150 kyr derived from thress cores PC27,...
