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Article Navigation >  Acta Sedimentologica Sinica  > 1997  >  15(S1): 41-45

Lei Zhenyu, Li Yongtie. High-frequency Cycles and High-resolution Sequence Stratigraphy of Ruyang Group, Mid-Proterozoic Era in Western Henan[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 41-45.
Citation: Lei Zhenyu, Li Yongtie. High-frequency Cycles and High-resolution Sequence Stratigraphy of Ruyang Group, Mid-Proterozoic Era in Western Henan[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 41-45.
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High-frequency Cycles and High-resolution Sequence Stratigraphy of Ruyang Group, Mid-Proterozoic Era in Western Henan

  • Research Institute of Petroleum Exploration and Developroent,Beijing 100083

  • Received Date: 1996-10-21
  • Ruyang Group in the western Henan can be divided into six third-order sequences. These sequences are made of some high-frequency sequence. The sequence 6 in them contains 9 parasequences sets and more than 36 parasequence. A parasoquence consistsof various sedimentary facies having upward-shallowing sequence, and is bounded by hiatus. The grain size is upward-coarseningand bed is upward thicking in parasequence. Geochemical data show As, Sb decrease and &13C increase in upward-shallowing se-quence. The character of the parasequence has relationship with to the sea-level change.
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    [2] 雷振宇.豫西中元古代汝阳群层序地层初步研究.地球科学，.1996,21(3):272-276.
    [3] 南京大学.地球化学，北京:科学出版社。1984,3210
    [4] 宋天锐.广东曲江一仁化晚二叠世地层的沉积相和元素变化.岩石地球化学，1983,2(1);87-96.
    [5] 钟华.山西五台山地区早元古代白云岩碳同位素演化及意义.中国科学(B辑),1993,23(10):1099~1104.
    [6] Jackson M. J.,Facies and sequence stratigraphic analysis in an in-tracratonic, thermal-relaxation basin: the earth Proterozoic LowerQuilalar Formation and Ballara Quartzite, mount. Isa. AustraliaSedimentary. 1990, 37(6):1053-1078
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  • Received:  1996-10-21

High-frequency Cycles and High-resolution Sequence Stratigraphy of Ruyang Group, Mid-Proterozoic Era in Western Henan

  • Research Institute of Petroleum Exploration and Developroent,Beijing 100083
  • Received Date: 1996-10-21

Abstract: Ruyang Group in the western Henan can be divided into six third-order sequences. These sequences are made of some high-frequency sequence. The sequence 6 in them contains 9 parasequences sets and more than 36 parasequence. A parasoquence consistsof various sedimentary facies having upward-shallowing sequence, and is bounded by hiatus. The grain size is upward-coarseningand bed is upward thicking in parasequence. Geochemical data show As, Sb decrease and &13C increase in upward-shallowing se-quence. The character of the parasequence has relationship with to the sea-level change.

Lei Zhenyu, Li Yongtie. High-frequency Cycles and High-resolution Sequence Stratigraphy of Ruyang Group, Mid-Proterozoic Era in Western Henan[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 41-45.
Citation: Lei Zhenyu, Li Yongtie. High-frequency Cycles and High-resolution Sequence Stratigraphy of Ruyang Group, Mid-Proterozoic Era in Western Henan[J]. Acta Sedimentologica Sinica, 1997, 15(S1): 41-45.
shu

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