Wang Qiansuo, Song Yougui
Shandong Provincial Key Laboratory of Water and Soil Conservation and Environmental Protection, College of Resources and Environment, Linyi University, Linyi 276000, China.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China.
Data Brief. 2018 Jan 31;17:297-304. doi: 10.1016/j.dib.2018.01.030. eCollection 2018 Apr.
This article presents clay minerals and major elements data of Miocene red clay from Zhuanglang core (ZL) from the eastern Longzhong Basin, China. The dataset including the contents of main clay minerals such as smectite, kaolinite, illite and chlorite and other important clay minerals parameters as illite crystallinity, Illite 5 Å/10 Å, kaolinite/(illite +chlorite) ratio and major elements and its ratio as SiO, AlO, MgO, NaO, KO, KO/AlO and SiO/AlO in the Mid-Miocene climatic optimum (MMCO). The X-ray diffraction (XRD) and X-ray Fluorescence (XRF) experiments were made at the State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences. The data provide the evidence for understanding the MMCO and its driving factors.
本文展示了来自中国陇中盆地东部庄浪岩芯（ZL）的中新世红粘土的粘土矿物和主要元素数据。该数据集包括蒙脱石、高岭石、伊利石和绿泥石等主要粘土矿物的含量，以及其他重要的粘土矿物参数，如伊利石结晶度、伊利石5Å/10Å、高岭石/（伊利石+绿泥石）比值，还有主要元素及其比值，如中新世气候适宜期（MMCO）的SiO₂、Al₂O₃、MgO、Na₂O、K₂O、K₂O/Al₂O₃和SiO₂/Al₂O₃。X射线衍射（XRD）和X射线荧光（XRF）实验在中国科学院地球环境研究所黄土与第四纪地质国家重点实验室进行。这些数据为理解中新世气候适宜期及其驱动因素提供了证据。
