Spatial-temporal distribution and tectonic setting of Mesozoic W-mineralized granitoids in the Xing-Meng Orogenic Belt, NE China

Xie, Wenchun; Zeng, Qingdong; Wang, Rui‐Liang; Wu, Jin‐Jian; Zhang, Zheming; Li, Fengchun; Zhang, Zhuang

doi:10.1080/00206814.2021.1961105

Cited by 11 publications

(30 citation statements)

References 204 publications

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“…The SGB, located in the southwestern part of NE China, extends north to Heilongjiang and Jilin provinces, and east to the Songliao Basin. This area is tectonically bordered by the HHF to the north, the Chifeng-Kangbao Fault (CKF) to the south and the Nenjiang-Balihan Fault (NBF) to the east (Xie et al 2021) (Fig. 1c).…”

Section: Geological Background and Samplingmentioning

confidence: 99%

“…Generally, W mineralization is associated with highly fractionated granites, as demonstrated by numerous cases worldwide (Singh & Singh, 2001;Fogliata et al 2012;Mao et al 2013;Huang & Jiang, 2014;Zhang, Y. et al 2017;Cao et al 2018Cao et al , 2020Jiang et al 2018;Yuan et al 2018;Steiner, 2019;Li, J. et al 2021;Xie et al 2021). It has been proposed that ore-forming elements may be concentrated during multiple stages of magmatic activity and then extracted by magmatic fluids (Che et al 2013;Harlaux et al 2018) or leached from granitoids and/or metamorphic rocks and transported by external (metamorphic or meteoric) fluids (Linnen & Williams-Jones, 1995;Vindel et al 1995;Vallance et al 2001).…”

Section: D Genetic Link Between the Narenwula Complex And W Mineraliz...mentioning

confidence: 99%

“…Numerous W deposits have been discovered in NE China, demonstrating the significant W metallogenic potential of this region (Ouyang et al 2015;Zeng et al 2015b;Liu et al 2016;Wang et al 2017;Zhang, X. B. et al 2017;Gao et al 2019;Wang, R. L. et al 2020;Xie et al 2021). At present, NE China is known to host 4 large, 18 medium and 17 small W deposits (Fig.…”

Section: Introductionmentioning

confidence: 97%

“…1c). Three W belts can be distinguished according to the distribution of the W deposits: the northern and central Great Xing'an Range W belt (NCGB), southern Great Xing'an Range W belt (SGB) and Lesser Xing'an-Zhangguangcai Range W belt (LXZB) (Xie et al 2021) (Fig. 1c).…”

Section: Introductionmentioning

confidence: 99%

“…1c). All of these W deposits are spatially and genetically related to granitic intrusions (Xie et al 2021). Although some studies have been conducted on the petrogenesis of these W-related granitic plutons, the petrogenesis of the these granitoids remains controversial (Mei et al 2015;Zeng et al 2015b;Wang et al 2017;Gao et al 2019;Yang et al 2019).…”

Section: Introductionmentioning

confidence: 99%

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Petrogenesis, W metallogenic and tectonic implications of granitic intrusions in the southern Great Xing’an Range W belt, NE China: insights from the Narenwula Complex

et al. 2022

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Extensive magmatism in NE China, eastern Central Asian Orogenic Belt, has produced multi-stage granitic plutons and accompanying W mineralization. The Narenwula complex in the southwestern Great Xing’an Range provides important insights into the petrogenesis, geodynamic processes and relationship with W mineralization. The complex comprises granodiorites, monzogranites and granite porphyry. Mafic microgranular enclaves are common in the granodiorites, and have similar zircon U–Pb ages as their host rocks (258.5–253.9 Ma), whereas the W-bearing granitoids yield emplacement ages of 149.8–148.1 Ma. Permian granodiorites are I-type granites that are enriched in large-ion lithophile elements and light rare earth elements, and depleted in high field strength elements and heavy rare earth elements. Both the mafic microgranular enclaves and granodiorites have nearly identical zircon Hf isotopic compositions. The results suggest that the mafic microgranular enclaves and granodiorites formed by the mixing of mafic and felsic magmas. W-bearing granitoids are highly fractionated A-type granites, enriched in Rb, Th, U and Pb, and depleted in Ba, Sr, P, Ti and Eu. They have higher W concentrations and Rb/Sr ratios, and lower Nb/Ta, Zr/Hf and K/Rb ratios than the W-barren granodiorites. These data and negative ϵHf(t) values (–6.0 to –2.1) suggest that they were derived from the partial melting of ancient lower crust and subsequently underwent extreme fractional crystallization. Based on the regional geology, we propose that the granodiorites were generated in a volcanic arc setting related to the subduction of the Palaeo-Asian Ocean, whereas the W-bearing granitoids and associated deposits formed in a post-orogenic extensional setting controlled by the Mongol–Okhotsk Ocean and Palaeo-Pacific Ocean tectonic regimes.

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Section: Geological Background and Samplingmentioning

confidence: 99%

Section: D Genetic Link Between the Narenwula Complex And W Mineraliz...mentioning

confidence: 99%

Section: Introductionmentioning

confidence: 97%

Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

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Petrogenesis, W metallogenic and tectonic implications of granitic intrusions in the southern Great Xing’an Range W belt, NE China: insights from the Narenwula Complex

et al. 2022

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Formation and evolution of multistage hydrothermal fluids in the Baishitouwa quartz–wolframite vein‐type deposit in the southern Great Xing'an Range tungsten belt, NE China: Constraints from individual fluid inclusion LA‐ICP‐MS analysis

et al. 2023

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Revealing hydrothermal evolution from the early oxide to late carbonate stages for quartz-wolframite vein-type deposits is essential for understanding the ore-forming process. In this study, we choose the Baishitouwa tungsten polymetallic deposit located in the southern Great Xing'an Range tungsten belt as a case study, and present detailed deposit geology and in situ fluid inclusion (FI) analyses including microthermometry, laser Raman spectra, and LA-ICP-MS microanalysis to address this issue. Four stages of hydrothermal activity were identified: (1) quartz-wolframite (I),(2) quartz-wolframite (II)-pyrite-chalcopyrite, (3) quartz-polymetallic sulphides, and (4) quartz-carbonate. Four types of FIs were recognized: CO 2 -rich, CO 2 -bearing, liquid-rich, and brine inclusions. Microthermometric data showed that the homogenization temperatures and salinities from the early to late stages are 380-460 C,

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Origin of the Narenwula quartz vein-type W deposit, Inner Mongolia, China: Insights from geochemistry of hosting granites, fluid inclusions, H-O-S isotopes, and wolframite trace elements

Wang,

Zhang,

Liu

et al. 2024

Journal of Asian Earth Sciences

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Spatial-temporal distribution and tectonic setting of Mesozoic W-mineralized granitoids in the Xing-Meng Orogenic Belt, NE China

Cited by 11 publications

References 204 publications

Petrogenesis, W metallogenic and tectonic implications of granitic intrusions in the southern Great Xing’an Range W belt, NE China: insights from the Narenwula Complex

Petrogenesis, W metallogenic and tectonic implications of granitic intrusions in the southern Great Xing’an Range W belt, NE China: insights from the Narenwula Complex

Formation and evolution of multistage hydrothermal fluids in the Baishitouwa quartz–wolframite vein‐type deposit in the southern Great Xing'an Range tungsten belt, NE China: Constraints from individual fluid inclusion LA‐ICP‐MS analysis

Origin of the Narenwula quartz vein-type W deposit, Inner Mongolia, China: Insights from geochemistry of hosting granites, fluid inclusions, H-O-S isotopes, and wolframite trace elements

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