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ZHANG Yingli. Peperite in the Jiufotang Formation of the Luanping Basin and Its Geological Implications[J]. Acta Sedimentologica Sinica, 2008, 26(1): 105-110.
Citation: ZHANG Yingli. Peperite in the Jiufotang Formation of the Luanping Basin and Its Geological Implications[J]. Acta Sedimentologica Sinica, 2008, 26(1): 105-110.

Peperite in the Jiufotang Formation of the Luanping Basin and Its Geological Implications

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  • Corresponding author: ZHANG Yingli
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2008-02-10
  • Based on observation in the field, this paper documents the sedimentary features and variations of Jiufotang Formation in the Luanping basin. A special kind of rock, namely, peperite, was identified and described in detail. Taking the geological setting of the basin into account, the author believes that the Luanping basin is a volcanic sedimentary basin. The intensive synsedimentary tectonic activity has resulted in the peperite in the Jiufotang Formation.
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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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  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2008-02-10

Peperite in the Jiufotang Formation of the Luanping Basin and Its Geological Implications

    Corresponding author: ZHANG Yingli

Abstract: Based on observation in the field, this paper documents the sedimentary features and variations of Jiufotang Formation in the Luanping basin. A special kind of rock, namely, peperite, was identified and described in detail. Taking the geological setting of the basin into account, the author believes that the Luanping basin is a volcanic sedimentary basin. The intensive synsedimentary tectonic activity has resulted in the peperite in the Jiufotang Formation.

ZHANG Yingli. Peperite in the Jiufotang Formation of the Luanping Basin and Its Geological Implications[J]. Acta Sedimentologica Sinica, 2008, 26(1): 105-110.
Citation: ZHANG Yingli. Peperite in the Jiufotang Formation of the Luanping Basin and Its Geological Implications[J]. Acta Sedimentologica Sinica, 2008, 26(1): 105-110.

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