Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China

Tian Mengyu; Di Yongjun; Li Shusheng; Zhang Sheng

doi:doi:10.11648/j.earth.20211006.18

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Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China

Tian Mengyu, Di Yongjun, Li Shusheng, Zhang Sheng

Published in Earth Sciences (Volume 10, Issue 6)

Received: 19 November 2021 Accepted: 7 December 2021 Published: 24 December 2021

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Abstract

The South China Block experienced intense tectonic–magmatic evolution during the Indosinian period, which was recorded by Indosinian granite and has attracted numerous researchers. This paper presents data on the geochronology and geochemistry of Darongshan biotite monzogranite. LA–ICP–MS U–Pb zircon analyses yielded a weighted average age of 250.1±1.6 Ma, which represents the magma crystallization age of the Early Triassic. According to petrographic observation, the main diagenetic minerals of Darongshan biotite monzogranite are quartz, K-feldspar, plagioclase, biotite, and small amounts of cordierite, tourmaline, and garnet. Darongshan biotite monzogranite is aluminum-rich and high in silica. It shows weak negative Eu anomalies (δEu=0.13–0.57) and depleted HREEs. Darongshan biotite monzogranite exhibits significant negative anomalies of high field strength elements (HFSE, e.g., Nb, Ta, Ti, and P) and positive anomalies of large-ion lithophile elements (LILE, e.g., Rb, Th, U, and Pb). Geochemical analyses suggested that Darongshan biotite monzogranite has undergone highly differentiated evolution. According to this study, Darongshan biotite monzogranite is an S-type granite, and its source material developed from the remelting of ancient crustal material. The Darongshan biotite monzogranite granite formed in the island arc environment of oceanic subduction and orogenic stage, further confirming the geological records of the remaining oceanic basin in Qinfang.

Published in	Earth Sciences (Volume 10, Issue 6)
DOI	10.11648/j.earth.20211006.18
Page(s)	325-331
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Zircon U-Pb, Geochemistry, Biotite Monzogranite, South China

References

[1]	Chappell B W (1999). Aluminium Saturation in I- and S-Type Granites and the Characterization of Fractionated Haplogranites. Lithos, 46 (3): 535-551.
[2]	Deng X G, Chen Z G, Li X H (2004). Shrimp U-Pb Zircon Dating of the Darongshan—Shiwandashan Granitoid Belt in Southeastern Guangxi, China. Geological Review, 50 (4): 426-432.
[3]	Irvine T N, Baragar W R A (1971). A Guide to the Chemical Classification of the Common Volcanic Rocks. Canadian Journal of Earth Sciences, 8 (5): 523-548.
[4]	Jiao S J, Guo J H, Peng S B (2013). Petrogenesis of Garnet in the DarongshanShiwandashan Granitic Suite of the South China Block and the Metamorphism of the Granulite Enclave. Acta Petrologica Sinica, 29: 1740-1758.
[5]	Kun L, Wancai S, Fei D (2017). The Petrology, Geochemical Characteristics and Origin of the Napeng Granite Mass Formed in Indo-China Period in the West of Guangdong Province. Journal of Geomechanics, 23 (3): 411-421.
[6]	Li Z X, Li X H (2007). Formation of the 1300-km-Wide Intracontinental Orogen and Postorogenic Magmatic Province in Mesozoic South China: A Flat-Slab Subductior Model. Geology, 35 (2): 179-182.
[7]	Li Y, Wei J, Santosh M, Tan J, Fu L, Zhao S (2016). Geochronology and Petrogenesis of Middle Permian S-Type Granitoid in Southeastern Guangxi Province, South China: Implications for Closure of the Eastern Paleo-Tethys. Tectonophysics, 682: 1-16.
[8]	Jochum K P, McDonough W F, Palme H, Spettel B (1989). Compositional Constraints on the Continental Lithospheric Mantle from Trace Elements in Spinel Peridotite Xenoliths. Nature, 340 (6234): 548-550.
[9]	Maniar P D, Piccoli P M (1989). Tectonic Discrimination of Granitoids. Geological Society of America Bulletin. Geological Society of America Bulletin, 101 (5): 635-643.
[10]	Nockolds S R, Allen R (1956). The Geochemistry of Some Igneous Rock Series—III. Geochimica et Cosmochimica Acta, 9 (1-2): 34-77.
[11]	Pearce J A, Harris N B W, Tindle A G (1984). Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks. Journal of Petrology, 25 (4): 956-983.
[12]	Yuanxi Q, Huanjiang C (1993). Professional Papers for the Gcological Structure of Yunkaidashan and Its Adjacent Areas. Beijing: Geological Publishing House.
[13]	Sun S S, McDonough W F (1989). Chemical and Isotope Systematics of Oceanic Basalts Implications for Mantle Composition and Processes. In Saunders AD, Ed Magmatism in Ocean Basins. Geological Society London Special Publications, 42: 313, 3456.
[14]	Sylvester P J (1998). Poat-Collisional Strongly Peraluminous Granites. Lithos, 45 (1-4): 29-44.
[15]	Taylor S R, McLennan S M (1985). The Continental Crust: Its Composition and Evolution. Oxford: Blackwell.
[16]	Mengyu T, Di Yongjun W S, Yilong J (2021). Geochemical Characteristics and Genesis of Biotite Monzogranite in Napeng Granite in Yunkai Area. Journal of Jilin University (Earth Science Edition), 51 (3): 749-766.
[17]	Wang C, Liang X Q, Zhou Y, Fu J G, Jiang Y, Dong C G, Xie Y H, Tong C X, Pei J X, Liu P (2015). Construction of Age Frequencies of Provenances on the Eastern Side of the Yinggehai basin: Studies of LA-ICP-MS U–Pb Ages of Detrital Zircons From Six Modern Rivers, Western Hainan, China. Earth Science Frontiers, 22: 277-289.
[18]	Xiaofeng Q, Zongqi W, Jie C, Zuohai F, Guiang H, Luozhong P (2013). Petrogenesis of Early Indosinian Granites From the Southwestern Segment of Qinfang Tectonic Belt, Southern Guangxi: Constraints From Zircon u-pb Chronology and Geochemistry. Journal of Jilin University (Earth Science Edition), 43 (5): 1471-1488.
[19]	Yang J H, Cawood P A, Du Y (2012b). Detrital record of Indosinian mountain building in SW China: provenance of the Middle Triassic turbidites in the Youjiang Basin. S, Huang H, Hu L S. Tectonophysics, 574-575: 105-117.
[20]	Wang Y, Fan W, Zhang G, Zhang Y (2013). Phanerozoic Tectonics of the South China Block: Key Observations and Controversies. Gondwana Research, 23 (4): 1273-1305.
[21]	Zhao L, Guo F, Fan W M, Li C W, Qin X F, Li H X (2012). Origin of the Granulite Enclaves in Indo-Sinian Peraluminous Granites, South China and Its Implication for Crustal Anatexis. Lithos, 150: 209-226.
[22]	Zhou X, Chen P, Xu X (2007). The Lithosphere Dynamical Evolution of Late Mesozoic Granites in Nanling Area, Beijing: Science Press.

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APA Style

Tian Mengyu, Di Yongjun, Li Shusheng, Zhang Sheng. (2021). Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China. Earth Sciences, 10(6), 325-331. https://doi.org/10.11648/j.earth.20211006.18

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ACS Style

Tian Mengyu; Di Yongjun; Li Shusheng; Zhang Sheng. Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China. Earth Sci. 2021, 10(6), 325-331. doi: 10.11648/j.earth.20211006.18

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AMA Style

Tian Mengyu, Di Yongjun, Li Shusheng, Zhang Sheng. Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China. Earth Sci. 2021;10(6):325-331. doi: 10.11648/j.earth.20211006.18

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@article{10.11648/j.earth.20211006.18,
  author = {Tian Mengyu and Di Yongjun and Li Shusheng and Zhang Sheng},
  title = {Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China},
  journal = {Earth Sciences},
  volume = {10},
  number = {6},
  pages = {325-331},
  doi = {10.11648/j.earth.20211006.18},
  url = {https://doi.org/10.11648/j.earth.20211006.18},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20211006.18},
  abstract = {The South China Block experienced intense tectonic–magmatic evolution during the Indosinian period, which was recorded by Indosinian granite and has attracted numerous researchers. This paper presents data on the geochronology and geochemistry of Darongshan biotite monzogranite. LA–ICP–MS U–Pb zircon analyses yielded a weighted average age of 250.1±1.6 Ma, which represents the magma crystallization age of the Early Triassic. According to petrographic observation, the main diagenetic minerals of Darongshan biotite monzogranite are quartz, K-feldspar, plagioclase, biotite, and small amounts of cordierite, tourmaline, and garnet. Darongshan biotite monzogranite is aluminum-rich and high in silica. It shows weak negative Eu anomalies (δEu=0.13–0.57) and depleted HREEs. Darongshan biotite monzogranite exhibits significant negative anomalies of high field strength elements (HFSE, e.g., Nb, Ta, Ti, and P) and positive anomalies of large-ion lithophile elements (LILE, e.g., Rb, Th, U, and Pb). Geochemical analyses suggested that Darongshan biotite monzogranite has undergone highly differentiated evolution. According to this study, Darongshan biotite monzogranite is an S-type granite, and its source material developed from the remelting of ancient crustal material. The Darongshan biotite monzogranite granite formed in the island arc environment of oceanic subduction and orogenic stage, further confirming the geological records of the remaining oceanic basin in Qinfang.},
 year = {2021}
}

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TY  - JOUR
T1  - Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China
AU  - Tian Mengyu
AU  - Di Yongjun
AU  - Li Shusheng
AU  - Zhang Sheng
Y1  - 2021/12/24
PY  - 2021
N1  - https://doi.org/10.11648/j.earth.20211006.18
DO  - 10.11648/j.earth.20211006.18
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 325
EP  - 331
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20211006.18
AB  - The South China Block experienced intense tectonic–magmatic evolution during the Indosinian period, which was recorded by Indosinian granite and has attracted numerous researchers. This paper presents data on the geochronology and geochemistry of Darongshan biotite monzogranite. LA–ICP–MS U–Pb zircon analyses yielded a weighted average age of 250.1±1.6 Ma, which represents the magma crystallization age of the Early Triassic. According to petrographic observation, the main diagenetic minerals of Darongshan biotite monzogranite are quartz, K-feldspar, plagioclase, biotite, and small amounts of cordierite, tourmaline, and garnet. Darongshan biotite monzogranite is aluminum-rich and high in silica. It shows weak negative Eu anomalies (δEu=0.13–0.57) and depleted HREEs. Darongshan biotite monzogranite exhibits significant negative anomalies of high field strength elements (HFSE, e.g., Nb, Ta, Ti, and P) and positive anomalies of large-ion lithophile elements (LILE, e.g., Rb, Th, U, and Pb). Geochemical analyses suggested that Darongshan biotite monzogranite has undergone highly differentiated evolution. According to this study, Darongshan biotite monzogranite is an S-type granite, and its source material developed from the remelting of ancient crustal material. The Darongshan biotite monzogranite granite formed in the island arc environment of oceanic subduction and orogenic stage, further confirming the geological records of the remaining oceanic basin in Qinfang.
VL  - 10
IS  - 6
ER  -

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Author Information

Tian Mengyu

School of Earth Science and Mineral Resources, China University of Geosciences, Beijing, China
Di Yongjun

School of Earth Science and Mineral Resources, China University of Geosciences, Beijing, China
Li Shusheng

Geology Team No. 4 of Guangxi Zhuang Autonomic Region, Nanning, China
Zhang Sheng

Remote Sensing Center of Guangxi, Nanning, China

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APA Style

Tian Mengyu, Di Yongjun, Li Shusheng, Zhang Sheng. (2021). Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China. Earth Sciences, 10(6), 325-331. https://doi.org/10.11648/j.earth.20211006.18

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ACS Style

Tian Mengyu; Di Yongjun; Li Shusheng; Zhang Sheng. Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China. Earth Sci. 2021, 10(6), 325-331. doi: 10.11648/j.earth.20211006.18

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AMA Style

Tian Mengyu, Di Yongjun, Li Shusheng, Zhang Sheng. Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China. Earth Sci. 2021;10(6):325-331. doi: 10.11648/j.earth.20211006.18

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@article{10.11648/j.earth.20211006.18,
  author = {Tian Mengyu and Di Yongjun and Li Shusheng and Zhang Sheng},
  title = {Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China},
  journal = {Earth Sciences},
  volume = {10},
  number = {6},
  pages = {325-331},
  doi = {10.11648/j.earth.20211006.18},
  url = {https://doi.org/10.11648/j.earth.20211006.18},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.earth.20211006.18},
  abstract = {The South China Block experienced intense tectonic–magmatic evolution during the Indosinian period, which was recorded by Indosinian granite and has attracted numerous researchers. This paper presents data on the geochronology and geochemistry of Darongshan biotite monzogranite. LA–ICP–MS U–Pb zircon analyses yielded a weighted average age of 250.1±1.6 Ma, which represents the magma crystallization age of the Early Triassic. According to petrographic observation, the main diagenetic minerals of Darongshan biotite monzogranite are quartz, K-feldspar, plagioclase, biotite, and small amounts of cordierite, tourmaline, and garnet. Darongshan biotite monzogranite is aluminum-rich and high in silica. It shows weak negative Eu anomalies (δEu=0.13–0.57) and depleted HREEs. Darongshan biotite monzogranite exhibits significant negative anomalies of high field strength elements (HFSE, e.g., Nb, Ta, Ti, and P) and positive anomalies of large-ion lithophile elements (LILE, e.g., Rb, Th, U, and Pb). Geochemical analyses suggested that Darongshan biotite monzogranite has undergone highly differentiated evolution. According to this study, Darongshan biotite monzogranite is an S-type granite, and its source material developed from the remelting of ancient crustal material. The Darongshan biotite monzogranite granite formed in the island arc environment of oceanic subduction and orogenic stage, further confirming the geological records of the remaining oceanic basin in Qinfang.},
 year = {2021}
}

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TY  - JOUR
T1  - Geochemical Characteristics and Genesis of Biotite Monzogranite in Southeastern Guangxi Province, South China
AU  - Tian Mengyu
AU  - Di Yongjun
AU  - Li Shusheng
AU  - Zhang Sheng
Y1  - 2021/12/24
PY  - 2021
N1  - https://doi.org/10.11648/j.earth.20211006.18
DO  - 10.11648/j.earth.20211006.18
T2  - Earth Sciences
JF  - Earth Sciences
JO  - Earth Sciences
SP  - 325
EP  - 331
PB  - Science Publishing Group
SN  - 2328-5982
UR  - https://doi.org/10.11648/j.earth.20211006.18
AB  - The South China Block experienced intense tectonic–magmatic evolution during the Indosinian period, which was recorded by Indosinian granite and has attracted numerous researchers. This paper presents data on the geochronology and geochemistry of Darongshan biotite monzogranite. LA–ICP–MS U–Pb zircon analyses yielded a weighted average age of 250.1±1.6 Ma, which represents the magma crystallization age of the Early Triassic. According to petrographic observation, the main diagenetic minerals of Darongshan biotite monzogranite are quartz, K-feldspar, plagioclase, biotite, and small amounts of cordierite, tourmaline, and garnet. Darongshan biotite monzogranite is aluminum-rich and high in silica. It shows weak negative Eu anomalies (δEu=0.13–0.57) and depleted HREEs. Darongshan biotite monzogranite exhibits significant negative anomalies of high field strength elements (HFSE, e.g., Nb, Ta, Ti, and P) and positive anomalies of large-ion lithophile elements (LILE, e.g., Rb, Th, U, and Pb). Geochemical analyses suggested that Darongshan biotite monzogranite has undergone highly differentiated evolution. According to this study, Darongshan biotite monzogranite is an S-type granite, and its source material developed from the remelting of ancient crustal material. The Darongshan biotite monzogranite granite formed in the island arc environment of oceanic subduction and orogenic stage, further confirming the geological records of the remaining oceanic basin in Qinfang.
VL  - 10
IS  - 6
ER  -

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