Published

2019-04-01

Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia

Características mineralógicas y significado petrogenético del clinopiroxeno y la hornblenda del complejo máfico de Wuhaolai en el Cratón del Norte de China, Mongolia Interior

DOI:

https://doi.org/10.15446/esrj.v23n2.66316

Keywords:

Wuhaolai mafic complex, genetic mineralogy, magmatic evolution, tectonic significance, margin of the North China Craton (en)
complejo máfico de Wuhaolai, mineralogía genética, evolución magmática, significación tectónica, margen del Cratón China del Norte. (es)

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Authors

  • Chen Wang Chang'an University - School of Earth Science and Resources
  • Liu Jianchao Chang'an University - School of Earth Science and Resources
  • zhang Haidong Chang'an University - School of Earth Science and Resources
  • Ge Jiakun Chang'an University - School of Earth Science and Resources
  • Xi Zhixuan Chang'an University - School of Earth Science and Resources
  • Wang Haoran Chang'an University - School of Earth Science and Resources
The Wuhaolai mafic complex is located in the north margin of the North China Craton (NCC), Inner Mongolia. To discuss the mineralogical features, magma evolution process, and tectonic setting of the complex, we analyzed the geochemical compositions of clinopyroxene and hornblende using an electron probe. The results revealed that the parental magma of this complex belonged to the intraplate alkaline basalt series. The normal zoning texture and the relation between Mg# and FeO, Al2O3, CaO, Na2O, SiO2 and Cr2O3 suggested that the clinopyroxenes of pyroxenite and gabbro crystallized from the same parental magma. The similar CaO content of clinopyroxenes indicated that the parental magma of the Wuhaolai complex may have suffered crustal contamination. Furthermore, the characteristics of hornblende demonstrated that the magma source was modified by fluids derived from subducted slab. Based on the value of Kdcpx (0.23–0.27), the equilibrium melt with clinopyroxene exhibited a relatively low Mg# (43–53), indicating that the parental magma was derived from the lithospheric mantle and underwent crystal fractionation. The gabbro crystallization temperature and pressure was found to be lower than that of pyroxenite, indicating that gabbro was formed at a lower depth than that of pyroxenite. Combining the tectonic setting discrimination diagram of clinopyroxene with the results of previous studies on the late Paleozoic intrusions near the research area, we proposed that the Wuhaolai complex was formed in an intraplate environment. The magma source was modified by fluids derived from the subducted slab during the subduction of the Paleo-Asian Ocean (PAO). After the PAO closure, the parental magma of the Wuhaolai complex was produced by the partial melting of the enriched lithospheric mantle

El complejo máfico de Wuhaolai está ubicado en el margen norte del Cratón del Norte de China (NCC), Mongolia Interior. Para analizar las características mineralógicas, el proceso de evolución del magma y el ajuste tectónico del complejo, analizamos las composiciones geoquímicas de clinopiroxeno y hornblenda utilizando una microsonda de electrones. Los resultados revelaron que el magma parental de este complejo pertenecía a la serie de basalto alcalino intraplaca. La textura normal de zonificación y la relación entre Mg # y FeO, Al2O3, CaO, Na2O, SiO2 y Cr2O3 sugirieron que los clinopiroxenos de piroxenita y gabbro se cristalizaron del mismo magma parental. El contenido similar de CaO de los clinopiroxenos indica que el magma parental del complejo Wuhaolai puede haber sufrido contaminación de la corteza. Además, las características de la hornblenda demostraron que la fuente de magma fue modificada por fluidos derivados de la losa subducida. Sobre la base del valor de Kdcpx (0.23–0.27), la masa fundida en equilibrio con clinopiroxeno exhibió un número de Mg relativamente bajo (43–53), lo que indica que el magma parental se derivó del manto litosférico y se sometió a un fraccionamiento de cristales. Se encontró que la temperatura y la presión de cristalización de gabbro eran más bajas que la de piroxenita, lo que indica que el gabro se formó a una profundidad más baja que la piroxenita. Combinando el diagrama de discriminación del ajuste tectónico del clinopiroxeno con los resultados de estudios previos sobre las últimas intrusiones del Paleozoico cerca del área de investigación, proponemos que el complejo Wuhaolai se forma en un entorno intraplaca. La fuente de magma fue modificada por fluidos derivados de la losa subducida durante la subducción del Océano Paleoasiático (PAO). Después del cierre de la PAO, el magma parental del complejo Wuhaolai se produjo mediante la fusión parcial del manto litosférico enriquecido

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APA

Wang, C., Jianchao, L., Haidong, zhang, Jiakun, G., Zhixuan, X. and Haoran, W. (2019). Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia. Earth Sciences Research Journal, 23(2), 133–146. https://doi.org/10.15446/esrj.v23n2.66316

ACM

[1]
Wang, C., Jianchao, L., Haidong, zhang, Jiakun, G., Zhixuan, X. and Haoran, W. 2019. Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia. Earth Sciences Research Journal. 23, 2 (Apr. 2019), 133–146. DOI:https://doi.org/10.15446/esrj.v23n2.66316.

ACS

(1)
Wang, C.; Jianchao, L.; Haidong, zhang; Jiakun, G.; Zhixuan, X.; Haoran, W. Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia. Earth sci. res. j. 2019, 23, 133-146.

ABNT

WANG, C.; JIANCHAO, L.; HAIDONG, zhang; JIAKUN, G.; ZHIXUAN, X.; HAORAN, W. Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia. Earth Sciences Research Journal, [S. l.], v. 23, n. 2, p. 133–146, 2019. DOI: 10.15446/esrj.v23n2.66316. Disponível em: https://revistas.unal.edu.co/index.php/esrj/article/view/66316. Acesso em: 16 apr. 2024.

Chicago

Wang, Chen, Liu Jianchao, zhang Haidong, Ge Jiakun, Xi Zhixuan, and Wang Haoran. 2019. “Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia”. Earth Sciences Research Journal 23 (2):133-46. https://doi.org/10.15446/esrj.v23n2.66316.

Harvard

Wang, C., Jianchao, L., Haidong, zhang, Jiakun, G., Zhixuan, X. and Haoran, W. (2019) “Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia”, Earth Sciences Research Journal, 23(2), pp. 133–146. doi: 10.15446/esrj.v23n2.66316.

IEEE

[1]
C. Wang, L. Jianchao, zhang Haidong, G. Jiakun, X. Zhixuan, and W. Haoran, “Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia”, Earth sci. res. j., vol. 23, no. 2, pp. 133–146, Apr. 2019.

MLA

Wang, C., L. Jianchao, zhang Haidong, G. Jiakun, X. Zhixuan, and W. Haoran. “Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia”. Earth Sciences Research Journal, vol. 23, no. 2, Apr. 2019, pp. 133-46, doi:10.15446/esrj.v23n2.66316.

Turabian

Wang, Chen, Liu Jianchao, zhang Haidong, Ge Jiakun, Xi Zhixuan, and Wang Haoran. “Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia”. Earth Sciences Research Journal 23, no. 2 (April 1, 2019): 133–146. Accessed April 16, 2024. https://revistas.unal.edu.co/index.php/esrj/article/view/66316.

Vancouver

1.
Wang C, Jianchao L, Haidong zhang, Jiakun G, Zhixuan X, Haoran W. Mineralogical features and petrogenetic significance of the clinopyroxene and hornblende of the Wuhaolai mafic complex in northern North China Craton, Inner Mongolia. Earth sci. res. j. [Internet]. 2019 Apr. 1 [cited 2024 Apr. 16];23(2):133-46. Available from: https://revistas.unal.edu.co/index.php/esrj/article/view/66316

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1. Haiqi Sun, Shaokui Pan, Hongyu Qin, Yimiao Liu, Xiaolong Wu. (2023). Age and Geochemistry of Zircon Megacrysts from Alluvial Deposits in the Huadian Area, Northeastern China. Minerals, 13(7), p.882. https://doi.org/10.3390/min13070882.

2. Linlin Hu, Shaokui Pan, Ren Lu, Jianping Zheng, Hongkun Dai, Anqi Guo, Li Yu, Haiqi Sun. (2022). Origin of gem-quality megacrysts in the Cenozoic alkali basalts from the Muling area, northeastern China. Lithos, 422-423, p.106720. https://doi.org/10.1016/j.lithos.2022.106720.

3. Shuimiao Fan, Bingfu Jin, Wei Yue, Lili Dang, Mengyao Wang, Qingxiang Kong. (2021). Type and genesis of amphibole in the Huanghe River and Changjiang River estuaries and significance of its provenance. Geosciences Journal, 25(5), p.575. https://doi.org/10.1007/s12303-020-0061-4.

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