Ground-penetrating radar study of beach-ridge deposits in Huangqihai Lake, North China: the imprint of washover processes

doi:10.1007/s11707-015-0501-z

Frontiers of Earth Science

2016, Vol. 10

Issue (1): 183-194 https://doi.org/10.1007/s11707-015-0501-z

本期目录

Ground-penetrating radar study of beach-ridge deposits in Huangqihai Lake, North China: the imprint of washover processes

Xin SHAN^1,²,Xinghe YU^1,^*(

),Peter D. CLIFT²,Chengpeng TAN¹,Shunli LI¹,Zhixing WANG¹,Dongxu SU¹

1. School of Energy Resources, China University of Geosciences (Beijing), Beijing 100083, China
2. Department of Geology and Geophysics, Louisiana State University, Baton Rouge, LA 70803, USA

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Abstract：

Determining the origin of beach ridges in lacustrine basins can often be problematic. The sedimentary processes responsible for formation of beach ridges on the north shore of Huangqihai Lake were investigated by using ground penetrating radar (GPR). A 400 MHz GPR antenna was used to achieve a high vertical resolution of 0.04–0.08 m. The radar stratigraphy was then determined using principles of seismic stratigraphy. The radar facies (RF) were determined by analyzing internal configuration and continuity of reflections, as well as reflection termination patterns.

The identified RF fall into three groups (inclined, horizontal and irregular). The inclined group consists of RF that display inclined reflections. The horizontal group consists of RF that exhibit predominantly horizontal reflections. In the irregular group, the reflections are typically weak. RF with reflections with gently landward dips in the shore-normal profile are interpreted as washover sheet deposits. RF with steeply landward-dipping and imbricated reflections are interpreted as washover lobes. Washover sheets develop when overwash fails to enter a significant body of water and sedimentation takes place entirely on the relatively flattened topography. Washover lobe development occurs when overwash enters a region in which topography dips steeply landward, and sedimentation takes place on the surface of washover sheets or previous washover lobes. The beach-ridge deposits are interpreted as being formed entirely from vertically and laterally stacked washover sheets and washover lobes. They were formed by wave-dominated processes and secondary overwash processes supplemented by longshore currents.

Key words： beach-ridge ground penetrating radar radar facies radar stratigraphy washover process

收稿日期: 2014-08-10 出版日期: 2015-12-25

Corresponding Author(s): Xinghe YU

引用本文:

. [J]. Frontiers of Earth Science, 2016, 10(1): 183-194.
Xin SHAN,Xinghe YU,Peter D. CLIFT,Chengpeng TAN,Shunli LI,Zhixing WANG,Dongxu SU. Ground-penetrating radar study of beach-ridge deposits in Huangqihai Lake, North China: the imprint of washover processes. Front. Earth Sci., 2016, 10(1): 183-194.

链接本文:

https://academic.hep.com.cn/fesci/CN/10.1007/s11707-015-0501-z
https://academic.hep.com.cn/fesci/CN/Y2016/V10/I1/183

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