TY - JOUR
T1 - Oxygen isotopic compositions and geological significance of zircons from the Yanshanian felsic intrusions in the Xidamingshan cluster, southeastern margin of the Youjiang fold belt, South China
T2 - In situ SHRIMP analysis
AU - Xiao, Chang Hao
AU - Shen, Yu Ke
AU - Liu, Huan
AU - Wei, Chang Shan
AU - Le, Xing Wen
AU - Fu, Bin
N1 - Publisher Copyright:
© Yanshi Xuebao/Acta Petrologica Sinica. All rights reserved.
PY - 2018
Y1 - 2018
N2 - The source and petrogenesis of the Late Cretaceous magmatism and associated Sn-W mineralization in the South China are yet well documented. This paper reports the oxygen isotope compositions of previously analyzed zircons from the Yanshanian felsic intrusions in the Xidamingshan cluster, along the southeastern margin of the Youjiang fold belt, Guangxi, South China. Zircon (Zrn) δ 18 O for quartz porphyry ranges from 5. 31‰ to 9. 31‰, VSMOW, averaging at 7. 61 ± 2. 17%. δ 18 OZm for beresitization biotite granite, fine biotite granite and medium biotite granite range from 7.11‰ to 9. 79‰(average = 8. 36 ± 1. 33‰), from 5. 06‰ to 9. 27‰ (average =7. 73 ±2. 23‰) and from 6. 27‰ to 9. 77‰ (average =8. 04 ± 1. 75‰), respectively. Monzonitic granite records a wide range in δ 18 O Zrn (5. 4‰ ~ 10. 99‰) with average of 7. 55 ±2. 77‰. The majorities are greater than the "mantle-like" values (δ 18 O: 5. 3 ±0. 6‰, 2σ). Except beresitization biotite granite, five samples have bimodal or multi-modal distribution characteristics and Hf-O plots of zircons have a negative correlation, indicating a crust-mantle interaction. Hf-0 isotopic compositions suggest that the source of the magma was mainly derived from partial melting of crustal material with input of mantle-derived components. The mantlederived melts imply that these melts not only provided necessary heat energy for crust partial melting, but also put got involved in the generation of granitic melts. Low oxygen fugacity as indicated by low Ce(IV)/Ce(III) ratios may be responsible for formation of large Pb-Zn-dominated skarn deposits. Our current research illustrates that combination of zircon Hf-0 isotope could more accurately trace the source of magma through distinguish juvenile components and parental magmas derived from reworking of pre-existing crustal material. And zircon O isotope is one of the most efficient techniques to study the metallogenetic regularity.
AB - The source and petrogenesis of the Late Cretaceous magmatism and associated Sn-W mineralization in the South China are yet well documented. This paper reports the oxygen isotope compositions of previously analyzed zircons from the Yanshanian felsic intrusions in the Xidamingshan cluster, along the southeastern margin of the Youjiang fold belt, Guangxi, South China. Zircon (Zrn) δ 18 O for quartz porphyry ranges from 5. 31‰ to 9. 31‰, VSMOW, averaging at 7. 61 ± 2. 17%. δ 18 OZm for beresitization biotite granite, fine biotite granite and medium biotite granite range from 7.11‰ to 9. 79‰(average = 8. 36 ± 1. 33‰), from 5. 06‰ to 9. 27‰ (average =7. 73 ±2. 23‰) and from 6. 27‰ to 9. 77‰ (average =8. 04 ± 1. 75‰), respectively. Monzonitic granite records a wide range in δ 18 O Zrn (5. 4‰ ~ 10. 99‰) with average of 7. 55 ±2. 77‰. The majorities are greater than the "mantle-like" values (δ 18 O: 5. 3 ±0. 6‰, 2σ). Except beresitization biotite granite, five samples have bimodal or multi-modal distribution characteristics and Hf-O plots of zircons have a negative correlation, indicating a crust-mantle interaction. Hf-0 isotopic compositions suggest that the source of the magma was mainly derived from partial melting of crustal material with input of mantle-derived components. The mantlederived melts imply that these melts not only provided necessary heat energy for crust partial melting, but also put got involved in the generation of granitic melts. Low oxygen fugacity as indicated by low Ce(IV)/Ce(III) ratios may be responsible for formation of large Pb-Zn-dominated skarn deposits. Our current research illustrates that combination of zircon Hf-0 isotope could more accurately trace the source of magma through distinguish juvenile components and parental magmas derived from reworking of pre-existing crustal material. And zircon O isotope is one of the most efficient techniques to study the metallogenetic regularity.
KW - Luowei W-Zn deposit
KW - SHRIMP
KW - Youjiang fold belt
KW - Zircon oxygen isotope
UR - http://www.scopus.com/inward/record.url?scp=85059990103&partnerID=8YFLogxK
M3 - Article
SN - 1000-0569
VL - 34
SP - 1441
EP - 1452
JO - Acta Petrologica Sinica
JF - Acta Petrologica Sinica
IS - 5
ER -