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WANG Jinfang, LI Yingjie, LI Hongyang, DONG Peipei. 2018: Zircon U-Pb dating of the Shijiangshan Late Jurassic-Early Cretaceous A-type granite in Xi Ujimqin Banner of Inner Mongolia and its tectonic setting. Geological Bulletin of China, 37(2-3): 382-396.
Citation: WANG Jinfang, LI Yingjie, LI Hongyang, DONG Peipei. 2018: Zircon U-Pb dating of the Shijiangshan Late Jurassic-Early Cretaceous A-type granite in Xi Ujimqin Banner of Inner Mongolia and its tectonic setting. Geological Bulletin of China, 37(2-3): 382-396.
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Zircon U-Pb dating of the Shijiangshan Late Jurassic-Early Cretaceous A-type granite in Xi Ujimqin Banner of Inner Mongolia and its tectonic setting

  • School of Natural Resources, Hebei Geological University, Shijiazhuang 050031, Hebei, China

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  • Received Date: October 19, 2016
  • Revised Date: March 26, 2017
  • Available Online: August 15, 2023
    Graphical Abstract
    • Abstract

  • Lying along the Hegenshan collisional orogenic suture zone in Xi Ujimqin Banner of Inner Mongolia, the Shijiangshan Atype granite intruded into Early Carboniferous Diyanmiao-Baiyinbulage ophiolite as well as Early Permian Shoushangou Formation and Dashizhai Formation, and consists mainly of monzogranites. The granite is geochemically characterized by high SiO2 (74.18%~77.16%), K2O (4.31%~5.07%), high absolute alkali values (Na2O+K2O=8.44%~9.16%), low Al2O3, CaO, MgO, TiO2, P2O5, Sr, Ba, Eu, Ti, P values, and higher Ga/Al (3.98~6.09), (Na2O+K2O)/CaO, K2O/MgO, TFeO/MgO, Rb/Nb, Y/Nb, Sc/Nb ratios. It is characterized by typical flat or slight right-inclined gull-wing shaped REE distribution patterns with obvious negative Eu anomalies (δEu=0.01~0.19). The Shijiangshan monzogranite exhibits typical geochemical characteristics of A-type granite, being significantly different from I, S and M type granites in geochemistry. According to the chemical subdivision diagrams of the A-type granitoids, the Shijiangshan A-type granite belongs to aluminous A2-type granitoid, formed and emplaced in a post-orogenic extension setting. LAICP-MS zircon U-Pb dating shows that the ages of the granite are 159.8±1.3Ma, 143.1±1.3Ma and 136.20±0.69Ma, suggesting that it was produced during Late Jurassic to Early Cretaceous and that the Hegenshan suture zone was at the post orogenic extension stage in the Late Jurassic-Early Cretaceous period.

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