Volume 3, Issue 5, October 2015, Pages: 256-260
Received: Aug. 10, 2015;
Accepted: Aug. 24, 2015;
Published: Sep. 2, 2015
Views 3954 Downloads 95
Zhao Xueqin, Institute of Environment and Resources, Southwest University of Science and Technology, Mianyang, China
Zhao Lijuan, School of Foreign Language and Cultures, Southwest University of Science and Technology, Mianyang, China
Wang Fudong, Institute of Environment and Resources, Southwest University of Science and Technology, Mianyang, China
The Quaternary of the Chengdu Basin contains abundant geological information. After being studied for decades, there are still some disputes over the Quaternary sedimentary environment and evolution and the filling sequence of basin, etc., on the whole even though some common perspectives have been reached with regard to stratigraphic architecture and structural characteristics. Particularly, more aspects must be further studied, including gravel characteristics and response to tectonic activity.
Research Status of the Quaternary Sedimentation in the Chengdu Basin, Science Research.
Vol. 3, No. 5,
2015, pp. 256-260.
Chen Zhirong, He Yinwu, 1990. A preliminary discussion on date determination of Guanghan clay and Chengdu clay with ~(14)C dates. Journal of Mountain Science, No.3, pp.167-173.
Cui Zhiqiang, Liu Dengzhong, Meng Qingmin, 2009.The origin of the Pleistocene gravel in western Sichuan depression. Geology of Chian, No.5, pp. 1065-1078.
Feng Jinliang, Zhao Zhenhong, Zhao Xiang et al., 2014. The Origin, Provenance, Age and Climatic Links of the Chengdu Clay: A Review. Journal of Mountain Science, Vol.32, No.55, pp.513-525
He Chengguang, Shao Zhaogang, Qian Cheng et al., 2011. Gravel fabric characteristics of Neogene conglomerate layers in the middle sector of the Longmenshan structural belt and its tectonic significance. Geology in China, No.6, pp. 1467-1476.
He Yinwu, 1987. On the formation of the Chengdu Basin (Plain). Regional Geology of China. No.2. pp. 169-176.
Li Chengsan, Wu Yansheng and Li Yongzhao, 1964. A Collection of Research Papers on the Remains of Quaternary Glaciers in China: The Remains of Quaternary Glaciers at the Eastern Slope of the South Section and Front of Longmen Mountain in Sichuan. Science Press, Beijing.
Li Daijun, 1980. Pleistocene Palynological assemblages in the Chengdu Plain. Acta Geological Sichuan, pp. 89-106
Li J, Xie S, Kuang M, 2001. Geomorphic evolution of the Yangtze Gorges and the time of their formation. Geomorphology, Vol.41, no.2–3, pp.125-135.
Li Yong, Hou Zhongjian, Si Guangyin et al., 2002. Cenozoic Tectonic sequence and tectonic events at the eastern margin of the Qinghai-Tibet plateau. Geology of China, Vol.29, No.1, pp.30-36.
Li Yong, Li Bing, Steffen D et al., 2006. Provenance Analysis and Drainage Evolution in Late Cenozoic Chengdu Basin on Eastern Margin of Tibetan Plateau. Acta Sedimentologica Sinica, No.3, pp. 309-320.
Li Yong, Li Yongzhao and Zhou Rongjun et al., 2002. Discovery of Quaternary fossil ice wedges in the Chengdu Plain and its palaeoclimatic significance. Journal of Geomechanics. No.4, pp.341-346.
Li Yong, Zhou Rongjun and Dersmore Alexander L. et al., 2006. Continental Dynamic Process and Geological Response at Eastern Edge of Qinghai-Tibet Plateau. Geological Publishing House, Beijing.
Li YongZhao, Shao ZhiGang, Li Daijun, 1984. The Quaternary Ice Age in the northwest edge of Sichuan Basin. Geological Publishing House, Beijing.
Li Zhongquan, Ying Danli, Li Hongkui et al., 2011. Evolution of the Western Sichuan Basin and Its superimposed characteristics, China. Acta Petrologica Sinica. No.8m pp.2362-2370.
Liang Bin, Zhu Bin, Wang Quanwei, et al. 2014. Quaternary geologocal and environment of Chengdu Plain. Geological Publishing House, Beijing.
Liang Bin,Wang Quanwei, Zhu Bing et al., 2013. Optically stimulated luminescence dating of the Chengdu clay in the west Sichuan basin. Quaternary Sciences, Vol.33, No.4, pp.823-828
Liang Mingjian;Li Dahu;Guo Hongmei, et al., 2014. Quaternary Tectonic Deformation and Geomorphologic Response Characteristics in the Southern Margin of Chengdu Basin. China Earthquake Engineering Journal, Vol.36, No.1, pp.98-106
Liu Shao, Zhang Shimin, Ding Rui, et al. 2015. Upper crustal folding of the 2013 Lushan earthquake area in southern Longmen Shan, China, insights from Late Quaternary fluvial terraces. Tectonophysics, No.639, pp.99-108.
Liu Xingshi, 1983. The Quaternary Period of Sichuan Basin. Sichuan Publishing House of Science & Technology, Chengdu.
Qiao Yansong, Zhao Zhizhong, Li Zengyue et al., 2007. Aeol ian origin of the red earth formation in the Chengdu plain. Quaternary Sciences, No.2, pp.286-294.
Thorp J, Dye D S, 1936. The chengtu clays—deposits of possible loessial origin in western and Northwestern Szechuan basin. Bulletin of the Geological Society of China, Vol.15, No.2, pp.225-242.
Wang Mingming Zhou Bengang Yang Xiaoping, et al., 2013. Characteristics of Late-Quaternary Activity and Seismic Risk of the Northeastern Section of the Longmenshan Fault Zone. Acta Geologica Sinica, Vol.87, No.6, pp.1674-1689
Xu Xiaosong, Liu Baojun, Xu Qiang, et al., 1997. Analysis and Geodynamics of Great Basins in West China. Geological Publishing House, Beijing.
Xu Zhonglu and Liu Yaping, 1982. A preliminary analysis of the development of the Western Sichuan Plain based on visual interpretation of landsat images. Geological Review, No.5, pp. 439-446.
Yang S, Fang X, Shi Z, et al., 2010. Timing and provenance of loess in the Sichuan Basin, southwestern China. Palaeogeography, Palaeoclimatology, Palaeoecology, Vol.292, No.1-2, pp.144-154.
Zeng Yunfu and Li Yong, 1994. On the sedimentary response to the effect of reverse thrust and nappe in Longmen Mountain—Taking the Chengdu Basin as an example. Mineralogy and Petrology, No.1, pp.58-66.
Zhang Zhuoyuan, Chen Xulun and Liu Shiqing et al., 2000. Origin and geological age of the Danling-Simong gravel bed. Journal of Mountain Science. No.S1, pp.8-16.
Zhou Xulun, 1986. The calcareous tuberculosis in Chengdu clay. Hydrogeology & Engineering Geology, No.4, pp.29-31.