Manganese, titanium and iron counts in marine sediment core MD01-2414 from the central Okhotsk Sea

The abundance of iron and manganese were detected by using non-destructive X-ray Fluorescence (XRF) scanning technique. Continuous downcore measurements of element variations were performed in the ITRAX XRF Core Scanner Laboratory, Department of Geosciences, National Taiwan University. All U-channel...

Full description

Bibliographic Details
Main Authors: Chou, Yu-Min, Jiang, Xiaodong, Lo, Li, Wang, Liang-Chi, Lee, Teh-Quei, Wang, Chun-Chieh, Pan, Yongxin, Zou, Jiangjun, Humbert, Fabien, Liu, Zhiqiang
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
AGE
DEPTH
sediment/rock
environmental magnetism
Giant piston corer
GPC
IMAGES VII - WEPAMA
Iron
Iron/Titanium ratio
log-Iron/Titanium ratio
log-Manganese/Titanium ratio
Manganese
Manganese/Titanium ratio
marine sediments
Marion Dufresne (1995)
MD012414
MD01-2414
MD122
Mid-Brunhes Transition
mid-Pleistocene transition
Okhotsk Sea
paleomagnetism
Sea ice
Sea of Ochotsk
Super-interglacial
terrigenous detritus
Titanium
X-ray fluorescence (XRF)
Okhotsk
okhotsk sea
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.932398
https://doi.org/10.1594/PANGAEA.932398
Description
Summary:The abundance of iron and manganese were detected by using non-destructive X-ray Fluorescence (XRF) scanning technique. Continuous downcore measurements of element variations were performed in the ITRAX XRF Core Scanner Laboratory, Department of Geosciences, National Taiwan University. All U-channels were scanned by using the 3 kW Mo source and were analyzed at 30 kV/24 mA, 2 mm resolution with a exposure time of 30 s. The count value of each element was calculated from element peak areas of original XRF spectra by the Q-Spec software provided by COX Analytical Systems.

Similar Items