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  1. No Access

    Article

    Geochemical records of palaeoclimatic changes in Weinan section since the last interglacial

    Weinan section consists of Holocene soil S0, last glacial loess L1, and last interglacial soil S1, furtherly L1 can be subdivided into three layers of loess (L1–1, L1–3, and L1–5), and two layers of weakly dev...

    Qizhong Wen, Guiyi Diao, Rongfen Jia, Jimin Sun… in Chinese Geographical Science (1997)

  2. No Access

    Article

    Organic geochemistry markers of climatic evolution in loess region of China

    Two hundred and thirty-five samples collected from Weinan loess section (L2 – S0) have been analyzed by TOC (total organic carbon) and pyrolysis hydrocarbons. The curve of TOC with depth has been set up and compa...

    Rongfen Jia, Zhao Lin, Youmei Liu, Qizhong Wen in Chinese Geographical Science (1997)