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LIU Kunfeng, WANG Yonghe, ZENG Zuoxun. Geological Characteristics of Tempestite from Cambrian Abuqiehai Formation in Middle Helan Mountain and Its Geological Significance[J]. Northwestern Geology, 2019, 52(1): 14-22. DOI: 10.19751/j.cnki.61-1149/p.2019.01.002
Citation: LIU Kunfeng, WANG Yonghe, ZENG Zuoxun. Geological Characteristics of Tempestite from Cambrian Abuqiehai Formation in Middle Helan Mountain and Its Geological Significance[J]. Northwestern Geology, 2019, 52(1): 14-22. DOI: 10.19751/j.cnki.61-1149/p.2019.01.002
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Geological Characteristics of Tempestite from Cambrian Abuqiehai Formation in Middle Helan Mountain and Its Geological Significance

  • 1. Sino Shaanxi Nuclear Industry Group Geological Survey Co, Ltd, Xi'an 710100, Shaanxi, China;

  • 2. Xi'an Center of China Geological Survey, Xi'an 710054, Shaanxi, China;

  • 3. School of Earth Sciences, China University of Geosciences, Wuhan 430074, Hubei, China

More Information
  • Received Date: March 04, 2018
  • Revised Date: August 28, 2018
  • Available Online: July 28, 2022
  • Published Date: March 04, 2019
    Graphical Abstract
    • Abstract
  • A suite of typical storm deposition has been discovered for the first time in Helanshan area of Ningxia, which was developed in the middle and lower parts of upper Cambrian. Bottom-erosion texture, bio-disturbed texture, imbricate-boulder texture and radial fabric can be found in these storm sediments, indicating a typical shallow-water storm deposition. The lower part of this formation consists of oolitic limestone, bamboo-like limestone and argillaceous banded limestone. The oolite shows an evident decline in the middle part, which mainly consists of calcirudite, algal limestone and argillaceous banded limestone. Dolomite lime appears in the top part of this formation, indicating a shallow subtidal sedimentary environment. The discovery of storm rock has a great significance for the reconstruction of middle and late Cambrian paleogeography and the comparison of regional strata in Helanshan area of Ningxia.
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    • References (54)
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