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Volume 22 Issue 3
Jun.  2011
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Long Shengxiang* (龙胜祥), Wu Shixiang (吴世祥), Li Hongtao (李宏涛), Bai Zhenrui (白振瑞), Ma Jinyu (马金钰), Zhang Hua (张华). Hybrid Sedimentation in Late Permian–Early Triassic in Western Sichuan Basin, China. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0186-5
Citation: Long Shengxiang* (龙胜祥), Wu Shixiang (吴世祥), Li Hongtao (李宏涛), Bai Zhenrui (白振瑞), Ma Jinyu (马金钰), Zhang Hua (张华). Hybrid Sedimentation in Late Permian–Early Triassic in Western Sichuan Basin, China. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0186-5

Hybrid Sedimentation in Late Permian–Early Triassic in Western Sichuan Basin, China

doi: 10.1007/s12583-011-0186-5
  • Received Date: 2018-07-15
  • Rev Recd Date: 2018-07-15
  • Publish Date: 2018-07-15
  • Mixed carbonate-siliciclastic sedimentation is common in the Upper Permian–Lower Triassic in the western Sichuan (四川) basin. The extensional movement was strong in the Late Permian, resulting in differential uplifting of fault blocks. During this period, there was an extensive retrogression. The Kangdian (康滇) ancient land progressive uplifted and enlarged, forming the major provenance of terrigenous clastics. In Changxingian age, mixed terrigenous-carbonate sedimentation was distributed in the area between Dafeishui (大飞水)-well Dashen (大深)-1-well Shoubao (寿保)-1 and Beichuan (北川)-well Guanji (关基). The terrigenous clastics sourced from Kangdian ancient land input into the relatively shallow water, resulting in an extensive limited platform-mixing tidal flat where moderate-thick laminated grey limestone, thin muddy limestone and purplish red sandy shale were de-posited...
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    沈阳化工大学材料科学与工程学院 沈阳 110142

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Hybrid Sedimentation in Late Permian–Early Triassic in Western Sichuan Basin, China

doi: 10.1007/s12583-011-0186-5

Abstract: Mixed carbonate-siliciclastic sedimentation is common in the Upper Permian–Lower Triassic in the western Sichuan (四川) basin. The extensional movement was strong in the Late Permian, resulting in differential uplifting of fault blocks. During this period, there was an extensive retrogression. The Kangdian (康滇) ancient land progressive uplifted and enlarged, forming the major provenance of terrigenous clastics. In Changxingian age, mixed terrigenous-carbonate sedimentation was distributed in the area between Dafeishui (大飞水)-well Dashen (大深)-1-well Shoubao (寿保)-1 and Beichuan (北川)-well Guanji (关基). The terrigenous clastics sourced from Kangdian ancient land input into the relatively shallow water, resulting in an extensive limited platform-mixing tidal flat where moderate-thick laminated grey limestone, thin muddy limestone and purplish red sandy shale were de-posited...

Long Shengxiang* (龙胜祥), Wu Shixiang (吴世祥), Li Hongtao (李宏涛), Bai Zhenrui (白振瑞), Ma Jinyu (马金钰), Zhang Hua (张华). Hybrid Sedimentation in Late Permian–Early Triassic in Western Sichuan Basin, China. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0186-5
Citation: Long Shengxiang* (龙胜祥), Wu Shixiang (吴世祥), Li Hongtao (李宏涛), Bai Zhenrui (白振瑞), Ma Jinyu (马金钰), Zhang Hua (张华). Hybrid Sedimentation in Late Permian–Early Triassic in Western Sichuan Basin, China. Journal of Earth Science, 2011, 22(3). doi: 10.1007/s12583-011-0186-5

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