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HE Yao-yan, NIU Zhi-jun, YANG Wen-qiang, SONG Fang, WANG Xiao-di, JIA Xiao-hui. Geochemical features of middle—upper Ordovician cherts series in centralsouthern Hunan and their implications for basin evolution during Ordovician[J]. GEOLOGY IN CHINA, 2016, 43(3): 936-952. DOI: 10.12029/gc20160317
Citation: HE Yao-yan, NIU Zhi-jun, YANG Wen-qiang, SONG Fang, WANG Xiao-di, JIA Xiao-hui. Geochemical features of middle—upper Ordovician cherts series in centralsouthern Hunan and their implications for basin evolution during Ordovician[J]. GEOLOGY IN CHINA, 2016, 43(3): 936-952. DOI: 10.12029/gc20160317
shu

Geochemical features of middle—upper Ordovician cherts series in centralsouthern Hunan and their implications for basin evolution during Ordovician

  • 1. China University of Geosciences Beijing, Beijing 100083, China;

  • 2. Key Laboratory for Paleontology and Coevolution of Life and Environment, CGS, Wuhan, 430205, Hubei, China;

  • 3. Wuhan Center of Geological Survey, CGS, Wuhan 430205, Hubei, China

Funds: 

Supported by Geological and Mineral Resources Survey & Evaluation Projects of China Geological Survey (No. 12120114039301, 12120113063600, 1212011120117).

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  • Received Date: June 22, 2015
  • Revised Date: September 22, 2015
  • Available Online: September 26, 2023
    Graphical Abstract
    • Abstract
  • Ordovician strata in central- southern Hunan consist of"finer clastic-chert- bearing series-coarser clastic rock", and their thickness varies regularly. Spatially, the thickness contours are distributed northeastwards nd meanwhile, the thickest tends to move southeastwards. In the study area, chert samples of Yanxi Formation in Lingkou section show high SiO2 values (89.08 %- 94.32%) and Al/(Al+Fe+Mn) ratios (0.52-0.79), and are characterized by slight enrichment of LREE and no obvious cerium and europium anomalies. Samples of equivalent formation in Daqiao section shows high SiO2 values (91.74 %-95.14%), and the Al/(Al+ Fe+Mn) ratios range from 0.34 to 0.56, with characteristics of LREE enrichment, intermittently negative cerium anomaly and no europium anomaly, and low Y/Ho ratios (20.65±1.63). Geochemical characteristics and discrimination diagrams of middle-upper Ordovician cherts in central-southern Hunan indicate that these rocks were bio-genetic and formed in an open continental margin. A correlation with equivalent formation in adjacent areas shows that these cherts have similar origins and sedimentary environments, which indicates that they formed in the same basin. Combined with the analysis of the iso-thickness diagram, it could be suggested that the basin in central-southern Hunan experienced the change from passive margin to foreland basin during Ordovician, and the cherts probably resulted from this transition. In addition, there is no obvious hydrothermal activity, suggesting the geodynamics that caused the uplift of Cathaysian block might have been located to the further southern or southeastern extension range of the cherts series in central-southern Hunan.
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