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- W2388122963 abstract "The Lower Jijicaozi group of early Permian age consists predominantly of mudstone and siltstone interbedded with sandstone. It was deposited in the distal slope of the Bogda retroarc collisional foreland basin, which developed along with the north Tianshan orogenic belt. Study of palaeocurrents and facies distribution patterns suggest that the slope was then facing south. More abundant and more varied soft-sediment structures than previously recognized in the lower Jijicaozi group were found during this study. They include loop beddings, hydroplastic folds, sand dikes, mushroom-like intrusions of sand or silt, dish-like water-escape, ball-and-pillow structures, fluidization conglomerate, pockets of fluidization conglomerate associated with diapirs, mixed layers, and syndepositional faults, all of which are consistent with seismogenic origin. They were formed in constrained horizons bounded by undeformed strata, suggesting that they are syndepositional. Field survey and statistical analysis of the fold hinges in the mixed layers and the axial planes of the pillow structures indicate that they are randomly distributed without any preferential direction. This observation demonstrates that all are earthquake-induced. As paleo-earthquakes in the Bogda retroarc collisional foreland basin originated during collision of the Tarim and Junggar blocks, our research on seismogenic soft-sediment structures may provide important clues toward understanding Permian formation of the Paleozoic north Tianshan orogenic belt and its related basins." @default.
- W2388122963 created "2016-06-24" @default.
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- W2388122963 date "2006-01-01" @default.
- W2388122963 modified "2023-09-25" @default.
- W2388122963 title "Early Permian seismically induced soft-sediment deformational structures in Bogda region, Xinjiang:stratigraphic records of earthquakes in the retroarc collisional foreland basin" @default.
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