The episodic geomorphological-sedimentary evolution of different basins in the Fenwei Graben and its tectonic implication

Author:

Hu Xiaomeng,Zhou Tianhang,Cai Shun

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous)

Reference53 articles.

1. An Z S, Kukala G, Proter S C, 1991a. Late Quaternary dust flow on the Chinese Loess Plateau. Catena, 18: 125–132.

2. An Z S, Kukla G J, Porter S C et al., 1991b. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years. Quaternary Research, 36(1): 29–36.

3. An Z S, Kutzbach J E, Prell W L et al., 2001. Evolution of Asian monsoons and phased uplift of the Himalaya- Tibetan Plateau since Late Miocene times. Nature, 411: 62–66.

4. Chen G D, 1987. On the geotectonic nature of the Fen-Wei rift system. Tectonophysics, 143(1–3): 217–223.

5. Chen M J, Hu X M, 2017. Regression-transgression cycles of paleolakes in the Fen River Graben Basin during the mid to late Quaternary and their tectonic implication. Frontiers of Earth Science, doi: 10.1007/s11707-016-0598-8.

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