Data for: Oligocene-Miocene (28-13 Ma) climato-tectonic evolution of the northeastern Qinghai-Tibetan Plateau evidenced by mineralogical and geochemical records of the Xunhua Basin

Published: 18 October 2018| Version 1 | DOI: 10.17632/tftgv523rc.1
Contributors:
Hanlie Hong,
Kaipeng Ji,
Wen Han,
Zhao Liu,
ke yin,
Thomas Algeo,
Qian Fang,
Chaowen Wang

Description

A total of 541 samples were collected at quasi-regular intervals of 3 to 4 m over a continuous stratigraphic interval of 1400 m spanning all four units of the Yangquangou section. Sampled lithologies include conglomerate, medium-coarse sandstone, fine sandstone, siltstone, and mudstone. Partial samples were selected according to lithological characteristics of detrital composition, grain size, and color for X-ray diffraction (XRD) and trace-element concentration measurements.

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