Volume 15 Issue 4
Dec.  2009
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Article Navigation >  Journal of Geomechanics  > 2009  >  15(4): 409-402
BAI Dao-yuan, ZHOU Ke-jun, MA Tie-qiu, et al., 2009. STUDY ON QUATERNARY TECTONIC-SEDIMENTARY EVOLUTION OF LUJIAO AREA, EAST EDGE OF YUANJIANG SAG, DONGTING BASIN. Journal of Geomechanics, 15 (4): 409-402.
Citation: BAI Dao-yuan, ZHOU Ke-jun, MA Tie-qiu, et al., 2009. STUDY ON QUATERNARY TECTONIC-SEDIMENTARY EVOLUTION OF LUJIAO AREA, EAST EDGE OF YUANJIANG SAG, DONGTING BASIN. Journal of Geomechanics, 15 (4): 409-402.
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STUDY ON QUATERNARY TECTONIC-SEDIMENTARY EVOLUTION OF LUJIAO AREA, EAST EDGE OF YUANJIANG SAG, DONGTING BASIN

  • Hunan Institute of Geology Survey, Changsha 410011, Hunan, China

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  • Received: 2009-08-18
  • Published: 2009-12-01
    Abstract
  • Quaternary Yuanjiang sag is an eastern one of the secondary tectonic units of the Dongting basin. Detailed geologic mapping and bore data were taken to reveal the Quaternary tectonic, sedimentary and geomorphic characteristics and tectonic-sedimentary evolution of Lujiao area, northeast Yuanjiang sag. The Honghu-Xiangyin fault and Rongjiawan fault formed in succession during Early Pleistocene, which caused that the west walls of the faults subsided and received alluvial and lacustrine deposits, while the east walls rose and were denuded. Eastern area of the sag uplifted and was denuded in the end of Early Pleistocene. The sag subsided and received alluvial and lacustrine deposits during early-middle Middle Pleistocene. The study area rose as a whole and was denuded during late Middle Pleistocene. The western main depressional area was stable or subsided weakly and formed clay deposits in Late Pleistocene, when east area rose by fits. In the same time of above tectonic uplift since late Middle Pleistocene, east of the area tilted westward and northward. The area was under tectonic stable state in Holocene, forming alluvial-lacustrine deposits in western Dongting lake area.

     

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