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                <identifier>oai:data.mendeley.com/tftgv523rc.1</identifier>
                <datestamp>2018-10-18T22:17:50Z</datestamp>
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    <dc:creator>Hong, Hanlie</dc:creator>
    <dc:title>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</dc:title>
    <dc:publisher>Mendeley Data</dc:publisher>
    <dc: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. </dc:description>
    <dc:subject>Geochemistry</dc:subject>
    <dc:subject>Mineralogy</dc:subject>
    <dc:contributor>Ji, Kaipeng</dc:contributor>
    <dc:contributor>Han, Wen</dc:contributor>
    <dc:contributor>Liu, Zhao</dc:contributor>
    <dc:contributor>yin, ke</dc:contributor>
    <dc:contributor>Algeo, Thomas</dc:contributor>
    <dc:contributor>Fang, Qian</dc:contributor>
    <dc:contributor>Wang, Chaowen</dc:contributor>
    <dc:type>Dataset</dc:type>
    <dc:identifier>doi:10.17632/tftgv523rc.1</dc:identifier>
    <dc:identifier>oai:data.mendeley.com/tftgv523rc.1</dc:identifier>
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    <dc:date>2018-10-18T22:17:50Z</dc:date>
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