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The genesis and mineralization significance of Guanyintang high Ba-Sr granitic intrusive rocks in the central section of the Taihang Mountains
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Juquan ZHANG1, 2, Chao CHEN2, *, Jing LU2, Lemin ZHANG2, Fuxiang ZHANG2, Haiquan GUO3, Tong ZHANG4, Cailong ZHANG3, Qichao FAN3, Huan XING3
Acta Mineralogica Sinica | 2026, 46(1) : 49 - 69
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Acta Mineralogica Sinica | 2026, 46(1): 49-69
The genesis and mineralization significance of Guanyintang high Ba-Sr granitic intrusive rocks in the central section of the Taihang Mountains
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Juquan ZHANG1, 2, Chao CHEN2, *, Jing LU2, Lemin ZHANG2, Fuxiang ZHANG2, Haiquan GUO3, Tong ZHANG4, Cailong ZHANG3, Qichao FAN3, Huan XING3
Affiliations
  • 1Postdoctoral Research Station of Hebei Bureau of Geology and Mineral Resources Exploration and Evelopment, Shijiazhuang Hebei 050051, China
  • 2College of Earth Sciences, Hebei GEO University, Shijiazhuang Hebei 052161, China
  • 3Hebei Bureau of Geology and Mineral Resources Exploration and Development, Shijiazhuang Hebei 050051, China
  • 4The Sixth Geological Brigade, Hebei Bureau of Geology and Mineral Resources Exploration and Development, Shijiazhuang Hebei 050051, China
Published: 2026-02-10 doi: 10.3724/j.1000-4734.2024.44.094
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A series of high Ba-Sr granitoids, developed in the Taihang Mountains region, are associated with a large amount of metal mineralization. To analyze their genesis is of great significance for studying the crust-mantle interaction and the evolution of its corresponding magmatic mineralization system in the destruction process of the North China Craton. This study takes the Guanyintang intrusion in the central section of the Taihang Mountains as an example to conduct zircon U–Pb geochronological, lithogeochemical, and genetic mineralogical researches of its different rocks. The research results show that main components of the Guanyintang intrusion are quartz monzonite, granodiorite, with minor diorite as the marginal phase of the intrusion. The compositions of dikes associated with the intrusion are consistent with those of main components of the Guanyintang intrusion. The diorite was formed at 125.2 Ma. Three measured ages for porphyritic quartz monzonite, granodiorite, and porphyritic granodiorite are 124.6 Ma,129.9 Ma, and 130.33 Ma, respectively. The Lu-Hf isotopic characteristics of zircons indicate that the Guanyintang intrusion was formed by the mixture of acidic magma produced by the partial melting of ancient crust and basic magma produced by the partial melting of lithospheric mantle. Characteristics of the zoning texture of orthoclase indicate that the Guanyintang high Ba-Sr granitoid was formed by the mixture of the granitic magma in the magma chamber and the mantle derived magma which were intruded into the acidic magma chamber in multiple pulsations.

high Ba-Sr granite  /  genetic mineralogy  /  petrogenesis  /  magmatic evolution  /  central section of the Taihang Mountains
Juquan ZHANG, Chao CHEN, Jing LU, Lemin ZHANG, Fuxiang ZHANG, Haiquan GUO, Tong ZHANG, Cailong ZHANG, Qichao FAN, Huan XING. The genesis and mineralization significance of Guanyintang high Ba-Sr granitic intrusive rocks in the central section of the Taihang Mountains[J]. Acta Mineralogica Sinica, 2026 , 46 (1) : 49 -69 . DOI: 10.3724/j.1000-4734.2024.44.094
Year 2026 volume 46 Issue 1
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doi: 10.3724/j.1000-4734.2024.44.094
  • Receive Date:2024-08-07
  • Online Date:2026-07-29
  • Published:2026-02-10
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  • Received:2024-08-07
Affiliations
    1Postdoctoral Research Station of Hebei Bureau of Geology and Mineral Resources Exploration and Evelopment, Shijiazhuang Hebei 050051, China
    2College of Earth Sciences, Hebei GEO University, Shijiazhuang Hebei 052161, China
    3Hebei Bureau of Geology and Mineral Resources Exploration and Development, Shijiazhuang Hebei 050051, China
    4The Sixth Geological Brigade, Hebei Bureau of Geology and Mineral Resources Exploration and Development, Shijiazhuang Hebei 050051, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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