南岭九嶷山地区砂子岭岩体成因与构造属性:来自锆石U-Pb年代学、岩石地球化学及Sr、Nd、Hf同位素证据

李剑锋; 付建明; 马昌前; 卢友月; 程顺波; 马丽艳; 秦拯纬

doi:10.3799/dqkx.2019.013

Volume 45 Issue 2

Feb. 2020

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Li Jianfeng, Fu Jianming, Ma Changqian, Lu Youyue, Cheng Shunbo, Ma Liyan, Qin Zhengwei, 2020. Petrogenesis and Tectonic Setting of the Shaziling Pluton in Jiuyishan Area, Nanling: Evidence from Zircon U-Pb Geochronology, Petrogeochemistry, and Sr-Nd-Hf Isotopes. Earth Science, 45(2): 374-388. doi: 10.3799/dqkx.2019.013

Citation:

Li Jianfeng, Fu Jianming, Ma Changqian, Lu Youyue, Cheng Shunbo, Ma Liyan, Qin Zhengwei, 2020. Petrogenesis and Tectonic Setting of the Shaziling Pluton in Jiuyishan Area, Nanling: Evidence from Zircon U-Pb Geochronology, Petrogeochemistry, and Sr-Nd-Hf Isotopes. Earth Science, 45(2): 374-388. doi: 10.3799/dqkx.2019.013

Citation:

Li Jianfeng, Fu Jianming, Ma Changqian, Lu Youyue, Cheng Shunbo, Ma Liyan, Qin Zhengwei, 2020. Petrogenesis and Tectonic Setting of the Shaziling Pluton in Jiuyishan Area, Nanling: Evidence from Zircon U-Pb Geochronology, Petrogeochemistry, and Sr-Nd-Hf Isotopes. Earth Science, 45(2): 374-388. doi: 10.3799/dqkx.2019.013

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Petrogenesis and Tectonic Setting of the Shaziling Pluton in Jiuyishan Area, Nanling: Evidence from Zircon U-Pb Geochronology, Petrogeochemistry, and Sr-Nd-Hf Isotopes

doi: 10.3799/dqkx.2019.013

Li Jianfeng^{1,2,3
,
,},
Fu Jianming^{1
,
,
,},
Ma Changqian²,
Lu Youyue¹,
Cheng Shunbo¹,
Ma Liyan¹,
Qin Zhengwei¹

1.
Wuhan Center of Geological Survey, China Geological Survey, Wuhan 430205, China
2.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
College of Urban and Environmental Science, Liaoning Normal University, Dalian 116029, China

Received Date: 2019-05-25
Publish Date: 2020-02-15

Abstract

Abstract

A study of LA-ICP-MS zircon U-Pb dating for Shaziling pluton composed of granodiorites and monzogranites from Jiuyishan area considered as a part of Nanling granite belt was carried out. The results of chronology indicate that the Shaziling pluton was formed during the early Yanshanian (151.9±1.1-154.1±1.2 Ma) instead of the Indosinian. The analyses of geochemistry indicate that the Shaziling pluton was characterized by rich silicon-alkali and poor calcium-magnesium with K₂O/Na₂O ratios of 1.37-2.65, Al₂O₃ of 0.93-1.09 and FeO^*/MgO ratios of 5.43-15.33 (average 7.14); The content of rare earth elements in the range of 186.75 to 413.17×10^-6 is significantly higher than the those of world average granite, which shows the right-leaning distribution of enriched light rare earth elements with obvious negative anomaly of Eu and δEu values of 0.095-0.224. These rocks are enriched in large ion lithophile elements (LILEs, e.g., Ga, Y, Nb, Zr, and Hf) and relatively depleted in high field strength elements (HFSEs, e.g., Ni, Cr, Eu, Ti, V, P, and Sr), with Ga/Al ratios of (245~582)×10^-6 (average 350×10^-6) and Zr+Nb+Ce+Y of (256.8-630.7)×10^-6 (average 441.95×10^-6), similar to geochemical features of A-type granites, which indicates the Shaziling pluton formed in the post- orogenic environment of the extensional tectonic system. Sr, Nd and Hf isotopes show that the Shaziling pluton has higher initial Sr isotope values of 0.71603 to 0.71817, lower ε_Nd(t) values of -6.8 to -7.4 and ε_Hf(t) values of 4.8 to -14.2, revealing that the source area occurred partial melting of crustal graywacke/pelite with a contribution of mantle materials during the diagenesis. Nd and Hf are relatively close in mode ages, with 1 498-1 546 Ma and 1 061-1 756 Ma, respectively, suggesting that the source rocks separated from the mantle reservoir during the Mesoproterozoic. Combined with the geological evolution of Nanling area that was in the tectonic setting of plate juncture zone and post-arc extension of Pacific plate, magmatism occurred in the Mesozoic Jiuyishan area in which the structure is relatively weak and there are a lot of new crustal materials with higher Lu/Hf and Sm/Nd isotope ratios. The Shaziling and Jiuyishan complex massif, similar to isotopic composition of A-type granites was formed by partial melting of the source area caused by mantle convection and upwelling of asthenosphere.
- A-type granites,
- zircon U-Pb dating,
- isotope,
- geochemistry,
- tectonic setting,
- Shaziling,
- Nanling

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References(82)

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Petrogenesis and Tectonic Setting of the Shaziling Pluton in Jiuyishan Area, Nanling: Evidence from Zircon U-Pb Geochronology, Petrogeochemistry, and Sr-Nd-Hf Isotopes

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