Seismites in a Proterozoic tidal succession, Singhbhum, Bihar, India

被引:104
作者
Bhattacharya, HN [1 ]
Bandyopadhyay, S [1 ]
机构
[1] Presidency Coll, Dept Geol, Calcutta 700073, W Bengal, India
关键词
Proterozoic; North Singhbhum Fold Belt; seismites; liquefaction; fluidization;
D O I
10.1016/S0037-0738(98)00051-7
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Early Proterozoic metasediments of the Chaibasa Formation (Galudih-Ghatsila-Dhalbhumgarh region, Singhbhum, Bihar, India) comprise a number of cyclic fining-upward prograding successions of tidalites. The tidalites show indications for earthquakes in the form of synsedimentary deformation features, apart from the structures due to high-energy wave action. Deformed cross-bedding, convolute laminations, synsedimentary faults, graben-like structures, sandstone dykes, pseudonodules and slump folds record the seismic activity. A gradual decline in the frequency of seismites and tsunami-related depositional features, in combination with an upward increase in thickness of the tidal cycles, are attributed to gradual diminishing of tectonic activity within the basin. (C) 1998 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:239 / 252
页数:14
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