Oxygen isotope compositions of quartz grains (4–16 μm) from Chinese eolian deposits and their implications for provenance
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://link.springer.com/content/pdf/10.1007/BF02959395.pdf
Reference29 articles.
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2. Ding, Z. L., Xiong, S. F., Sun, J. M. et al., Pedostratigraphy and paleomagnetism of a ∼7.0 Ma eolian loess-red clay sequence at Lingtai, Loess Plateau, north-central China and the implications for paleomonsoon evolution, Palaeogeography, Palaeoclimatology, Palaeoecology, 1999, 152: 49–66.
3. Ding, Z. L., Sun, J. M., Yang, S. L. et al., Preliminary magnetostratigraphy of a thick eolian red clay-loess sequence at Lingtai, the Chinese Loess Plateau, Geophysical Research Letters, 1998, 25: 1225–1228.
4. Ding, Z. L., Sun, J. M., Liu, T. S. et al., Wind-blown origin of the Pliocene red clay formation in the central Loess Plateau, China, Earth and Planetary Science Letters, 1998, 161: 135–143.
5. Ding, Z. L., Sun, J. M., Yang, S. L. et al., Geochemistry of the Pliocene red clay formation in the Chinese Loess Plateau and implications for its origin, source provenance and paleoclimate change, Geochimica et Cosmochimica Acta, 2001, 65(6): 901–913.
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