Mounded seismic units in the modern canyon system in the Shenhu area, northern South China Sea: Sediment deformation, depositional structures or the mixed system?
Mounded seismic units in the modern canyon system in the Shenhu area, northern South China Sea: Sediment deformation, depositional structures or the mixed system?
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南海北部神狐海域现代峡谷体系中的丘状地震单元:沉积物变形、沉积构造还是混合体系?
DOI:
10.1007/s13131-022-2002-8
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发表时间:
2022-09
期刊:
影响因子:
--
通讯作者:
Liu Lejun
中科院分区:
文献类型:
--
作者:
Li Xishuang;Zhang Chengyi;Liu Baohua;Liu Lejun
The canyon system, including 17 small slope-confined canyons in the Shenhu area, northern South China Sea, is significantly characterized by mounded or undulating features on the canyon flanks and canyon heads. However, the mechanism underlying the formation of these features has yet to be elucidated. In previous studies, most of them were interpreted as sediment deformation on the exploration seismic profiles. In this paper, we collected high-resolution bathymetric data, chirp profiles and geotechnical test data to investigate their detailed morphology, internal structures, and origin. The bathymetric data indicated that most mounded seismic units have smooth seafloors and are separated by grooves or depressions. The distance between two adjacent mounded units is only hundreds of meters. On chirp profiles, mounded seismic units usually exhibit chaotic reflections and wavy reflections, of which the crests migrate upslope. The slope stability analysis results revealed that the critical angle of the soil layers in the study area tends to be 9°, indicating that most mounded seismic units on the canyon flanks and heads are stable at present. The terrain characteristics and seismic configurations combined with the slope stability analysis results indicated that most mounded seismic units are not sediment deformation but depositional structures or mixed systems composed of deformation and depositional structures.
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DOI:
10.1007/978-3-642-57916-5_3
发表时间:
1965
期刊:
--
影响因子:
--
作者:
D. Mumford;J. Fogarty;F. Kirwan
通讯作者:
D. Mumford;J. Fogarty;F. Kirwan
影响因子:
2.1
作者:
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通讯作者:
D. O'leary;E. Laine
影响因子:
3
作者:
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通讯作者:
Rachel E. Brackenridge
影响因子:
3.5
作者:
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通讯作者:
C. Gong;Yingmin Wang;Weilin Zhu;Weiguo Li;Qiang Xu
影响因子:
2
作者:
M. Gee;R. Gawthorpe;S. J. Friedmann
通讯作者:
M. Gee;R. Gawthorpe;S. J. Friedmann