赣西北小九宫-沙店白垩纪花岗岩的岩石成因及构造意义

王艳; 马昌前; 王连训; 刘园园

doi:10.3799/dqkx.2019.116

Volume 45 Issue 4

Apr. 2020

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Article Navigation > Earth Science > 2020 > 45(4): 1115-1135

Wang Yan, Ma Changqian, Wang Lianxun, Liu Yuanyuan, 2020. Petrogenesis and Tectonic Implications of the Cretaceous Granites from Xiaojiugong-Shadian, Northwest Jiangxi Province. Earth Science, 45(4): 1115-1135. doi: 10.3799/dqkx.2019.116

Citation:

Wang Yan, Ma Changqian, Wang Lianxun, Liu Yuanyuan, 2020. Petrogenesis and Tectonic Implications of the Cretaceous Granites from Xiaojiugong-Shadian, Northwest Jiangxi Province. Earth Science, 45(4): 1115-1135. doi: 10.3799/dqkx.2019.116

Citation:

Wang Yan, Ma Changqian, Wang Lianxun, Liu Yuanyuan, 2020. Petrogenesis and Tectonic Implications of the Cretaceous Granites from Xiaojiugong-Shadian, Northwest Jiangxi Province. Earth Science, 45(4): 1115-1135. doi: 10.3799/dqkx.2019.116

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Petrogenesis and Tectonic Implications of the Cretaceous Granites from Xiaojiugong-Shadian, Northwest Jiangxi Province

doi: 10.3799/dqkx.2019.116

Wang Yan^{1
,
,},
Ma Changqian^{2, 3
,
,
,},
Wang Lianxun^{2, 3},
Liu Yuanyuan⁴

1.
Guangdong Nonferrous Metals Geological Exploration Institution, Guangzhou 510080, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
4.
Faculty of Geosciences and Environmental Engineering, Southwest Jiaotong University, Chengdu 611756, China

Received Date: 2019-05-14
Publish Date: 2020-04-15

Abstract

Abstract

Many Late Mesozoic granites occur in northwest Jiangxi Province and northeast Hunan Province, which constitute a NEE-trending magmatic belt together with the Late Mesozoic granites in the Middle and Lower Yangtze regions. In this paper, it presents the petrogenesis and tectonic implications, based on the systematic petrographical, zircon U-Pb geochronological, geochemical and isotopic analyses of two representative samples from the Xiaojiugong and Shadian granites. The Xiaojiugong and Shadian intrusions principally consist of medium to coarse-grained porphyritic biotite monzogranite. LA-ICP-MS zircon U-Pb dating yields magma crystallization ages of 124±1 Ma for the Xiaojiugong intrusion and 125±1 Ma for the Shadian intrusion. The two intrusions emplaced in the period of Late Yanshanian. The Xiaojiugong and Shadian granites are all characterized by high-K, calc-alkaline and low contents of Fe₂O₃^T and MgO, indicating they are mainly weakly peraluminous granites. They show similar distribution patterns of REE and trace elements, i.e. enrichment in LREE and large-ion lithophile elements of K, Rb, Th and U, depletion in Ba, Sr, P and high field strength elements of Nb, Ta and Ti, and pronounced negative Eu anomalies (Eu/Eu^*=0.17-0.50). Major and trace elements show that the Xiaojiugong and Shadian granites are high-K calc-alkaline Ⅰ-type granites. The Xiaojiugong granites have ε_Nd(t) values of -8.06 to -6.20 and two-stage model ages (T_DM2) of 1.42-1.57 Ga. The Shadian granites have ε_Nd(t) values of -6.51 to -6.08 and the corresponding T_DM2 of 1.42-1.45 Ga. The Sr-Nd isotopic composition and geochemical characteristics of the Xiaojiugong and Shadian granites suggest the main origin of lower crust. Their source might be the Mesoproterozoic neutral-basic igneous rocks. The Xiaojiugong and Shadian granites passively emplaced through expansion of the dikes. Combined with the regional tectonic background, the granites formed in extensional environment, and upwelling mantle probably provided a continuous heat source for the partial melting of lower crustal igneous rocks. The magma experienced a significant process of fractional crystallization during upwelling. A handful of microgranular enclaves and surrounding rock xenoliths in the granites reflect that the granitic magma might have been weekly contaminated when rising. Regional comparison shows that, from Early Yanshanian to Late Yanshanian, the pressure of the granitic magma source decreased significantly in the northwest Jiangxi and northeast Hunan. This might indicate that the crust had undergone significant thinning in the period of Late Mesozoic.
- zircon U-Pb geochronology,
- geochemistry,
- Sr-Nd isotope,
- Ⅰ-type granite,
- petrogenesis,
- tectonic implication,
- petrology

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References(67)

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Petrogenesis and Tectonic Implications of the Cretaceous Granites from Xiaojiugong-Shadian, Northwest Jiangxi Province

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