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WANG Kai-kai, LIU Chuan-peng, DENG Jun, LIANG Cheng, LIU Tong. 2021. Geochemical and Mineralogical Characteristics of Hornblende in Western Shandong and Their Geological Significance. Acta Geoscientica Sinica, (6): 771-787. doi: 10.3975/cagsb.2021.091402
Citation: WANG Kai-kai, LIU Chuan-peng, DENG Jun, LIANG Cheng, LIU Tong. 2021. Geochemical and Mineralogical Characteristics of Hornblende in Western Shandong and Their Geological Significance. Acta Geoscientica Sinica, (6): 771-787. doi: 10.3975/cagsb.2021.091402
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Geochemical and Mineralogical Characteristics of Hornblende in Western Shandong and Their Geological Significance

  • 1. The 7th Institute of Geology & Mineral Exploration of Shangdong Province, Linyi, Shangdong 276006;

  • 2. Key Laboratory of Diamond Mineralization Mechanism and Exploration, Shandong Provincial Bureau of Geology & Mineral Resources, Linyi, Shandong 276006;

  • 3. Academician Workstation of Diamond Metallogenic Mechanism and Exploration in Shandong Province, Linyi, Shangdong 276006

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  • Corresponding author: LIU Chuan-peng  
Received Date:  23 June 2021
Revised Date:  29 August 2021
    Abstract
  • Dike groups are formed under extensional background and are an important indicator for tracking mantle source characteristics, and continental and supercontinental rupture.Hornblende rocks in western Shandong enable the evaluation of Paleoproterozoic magma source and tectonic evolution.In the present study, petrographic, whole-rock geochemical, and in situ analyses of amphibole and biotite in the western Shandong area were carried out.Hornblende rocks with intraplate tectonic setting from enriched mantle were employed.According to an analysis of the origin of hornblende and biotite, both were of mantle origin.The crystallization temperature of hornblende was 702~781℃.Further, hornblende had a crystallization pressure of 29.8~228.8 MPa, crystallization depth of approximately 1~7.5 km, and its oxygen fugacity varied from NNO+2.68 to NNO+3.35 during crystallization.As the U-Pb age of hornblende apatite was (1817±35) Ma, (1817±35) Ma in the western Shandong area was considered to be in the in-plate tensile environment, where mantle derived magma transgression occurs, and the stage of continental cracking is entered.
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