• The Core Journal of China
  • Included in Chinese Scientific and Technical Papers and Citations Database
  • Included in Chinese Science Citation Database (CSCD)
  • Included in Chemical Abstracts (CA)
  • Included in Scopus
Advanced Search
Wang Jian, Zhuang Ruli, Lao Ketong, Long Guohua. DIVISION AND GEOLOGICAL IMPLICATIONS OF CALCAREOUS AIGAL MORPHOLOGICAL GROUPS AND ENVIRONMENTAL ZONES IN THE LOWER CAMBRIAN QINGXUDONG FORMATION,HUAYUAN DISTRICT,WESTERN HUNAN[J]. Sedimentary Geology and Tethyan Geology, 1990, 10(3): 9-19.
Citation: Wang Jian, Zhuang Ruli, Lao Ketong, Long Guohua. DIVISION AND GEOLOGICAL IMPLICATIONS OF CALCAREOUS AIGAL MORPHOLOGICAL GROUPS AND ENVIRONMENTAL ZONES IN THE LOWER CAMBRIAN QINGXUDONG FORMATION,HUAYUAN DISTRICT,WESTERN HUNAN[J]. Sedimentary Geology and Tethyan Geology, 1990, 10(3): 9-19.

DIVISION AND GEOLOGICAL IMPLICATIONS OF CALCAREOUS AIGAL MORPHOLOGICAL GROUPS AND ENVIRONMENTAL ZONES IN THE LOWER CAMBRIAN QINGXUDONG FORMATION,HUAYUAN DISTRICT,WESTERN HUNAN

More Information
  • Published Date: June 29, 1990
  • The bioherms are widespread during deposition of the Lower Cambrian Qingxudong Formation in the Huayuan district, western Hunan. They comprise nineteen genera and species of calcareous algae and may be subdivided into four groups and seven subgroups according to their morphologies: (1) botryoidal group; (2) dendritic group including: (a) fine and short subgroup, (b) clustered and ball-shaped subgroup, and (c) dendritic subgroup; (3) tubular group including: (a) fan-shaped tubular subgroup, (b) isolated and scattered tubular subgroup, (c) clustered tubular subgroup, (d) coiled-massive and spiral subgroup, and (4) blanket hair-like group.
    One or several algal morphological groups and/or subgroups can be assigned to either of four algal environmental zones of the bioherms, where the distribution of energy differs from that in the organic reefs. For example, the low-energy zone occurs at the bottom and periphery of the bioherms, whereas relatively high-energy in the central part of the bioherms, and very high-energy zone on the top of the bioherms. No differences in energy have been identified in the environments around the bioherms; all the algal environmentsl are confined to the deeper-water low-energy environments in the study area.
  • Related Articles

    [1]CHEN Fu-gui, KANG Kong-yue, CHEN Bei-zhan, YANG Wei, ZHANG Jie, CHEN Lin, ZHU Da-wei, LI Tong-xuan. Provenance analysis of the Middle-Lower Jurassic Yarkant Group in the Mazar tectonic mélange zone in western Kunlun Mountains[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(2): 66-78.
    [2]LI Yong, HOU Ming-cai, KANG Kong-yue, ZHANG Jie, CHEN Lin. Sedimentary environments of the B Formation of the Upper Carboniferous Qiati'er Group in the Tianshuihai-Mazar block, western Kunlun Mountains[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(1): 55-61.
    [3]LIANG Wei, MOU Chuan-long, ZHOU Ken-ken, GE Xiang-ying. Sedimentary environments of the Lower Cambrian source rocks in central Hunan[J]. Sedimentary Geology and Tethyan Geology, 2011, 31(4): 34-39.
    [4]JIN Can-hai, ZHU Tong-xing, YU Yuan-shan, ZHOU Bang-guo, FENG Xin-tao. Stratigraphic characteristics and sedimentary environments of the Upper Triassic Rola Kangri Group Complex on the northern margin of North Qiangtang continental block[J]. Sedimentary Geology and Tethyan Geology, 2010, 30(2): 39-46.
    [5]YANG Shao-xiang, PANG Ke-tong. Mineralization model for the manganese deposits in northwestern Hunan: An example from Minle manganese deposit in Huayuan,Hunan[J]. Sedimentary Geology and Tethyan Geology, 2006, 26(2): 72-80.
    [6]PEI Zhong-chao, ZHU Guang-bin, YANG Zhen-jun. The biotic fossils from the Upper Carboniferous Zhouying Formation in the Xichuan district,southwestern Henan[J]. Sedimentary Geology and Tethyan Geology, 2004, 24(2): 63-69.
    [7]LI Zhong-xiong, WANG Jian, DUAN Tai-zhong, GAO Yong-hua. Sequence stratigraphic division of the Upper Sinian-Lower Cambrian strata in the Cili-Dayong region, northwestern Hunan[J]. Sedimentary Geology and Tethyan Geology, 2003, 23(4): 27-33.
    [8]CAI Xiong-fei, LI Chang-an, ZHAN Che-sheng, GU Yan-sheng. The construction and significance of the Yanguoxia Formation on the southern margin of the Minhe Basin,Gansu[J]. Sedimentary Geology and Tethyan Geology, 1999, 19(3): 16-20.
    [9]Jiang Maosheng, Sha Qing'an. ALGAL LIMESTONES AND THEIR SEDIMENTARY FACIES IN THE ZHANGXIA FORMATION (MIDDLE CAMBRIAN),NORTH JIANGSU-WEST SHANDONG REGION[J]. Sedimentary Geology and Tethyan Geology, 1996, 16(5): 12-17.
    [10]Liu Baojun, Yu Guangming, Chen Chengsheng. OPHIOLITIC SUBMARINE FANS AND THEIR PIATETECTONIC SETTINGS IN THE XIGAZE GROUP ALONG THE YARLUNG ZANGBO SUTURE ZONE IN XIZANG[J]. Sedimentary Geology and Tethyan Geology, 1993, 13(2): 13-24.

Catalog

    Article views (74) PDF downloads (69) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return