黄陵隆起片麻岩和花岗岩的<sup>40</sup>Ar/<sup>39</sup>Ar年龄及其构造意义

吴阳; 沈传波; 邱华宁

doi:10.3799/dqkx.2022.501

Volume 49 Issue 2

Feb. 2024

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Wu Yang, Shen Chunbo, Qiu Huaning, 2024. 40Ar/39Ar Ages of Gneiss and Granite from Huangling Uplift and Their Tectonic Significance. Earth Science, 49(2): 700-711. doi: 10.3799/dqkx.2022.501

Citation:

Wu Yang, Shen Chunbo, Qiu Huaning, 2024. ⁴⁰Ar/³⁹Ar Ages of Gneiss and Granite from Huangling Uplift and Their Tectonic Significance. Earth Science, 49(2): 700-711. doi: 10.3799/dqkx.2022.501

Wu Yang, Shen Chunbo, Qiu Huaning, 2024. 40Ar/39Ar Ages of Gneiss and Granite from Huangling Uplift and Their Tectonic Significance. Earth Science, 49(2): 700-711. doi: 10.3799/dqkx.2022.501

Citation:

Wu Yang, Shen Chunbo, Qiu Huaning, 2024. ⁴⁰Ar/³⁹Ar Ages of Gneiss and Granite from Huangling Uplift and Their Tectonic Significance. Earth Science, 49(2): 700-711. doi: 10.3799/dqkx.2022.501

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⁴⁰Ar/³⁹Ar Ages of Gneiss and Granite from Huangling Uplift and Their Tectonic Significance

doi: 10.3799/dqkx.2022.501

Wu Yang^{1
,
,},
Shen Chunbo^{1, 2
,
,
,},
Qiu Huaning^{1, 2}

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China

Received Date: 2022-12-29
Publish Date: 2024-02-25

Abstract

Abstract

The Huangling uplift, located in the front of the northeast corner of the Sichuan Basin, is composed mainly of Huangling granite. The granite is the geological record of the Jinning orogeny and the Rodinia supercontinent cracking in the Yangtze block, and it is critical for understanding the tectonic evolution and magmatic activity of the Yangtze block. To determine the formation time of the Huangling granite, abundant chronological data were published using isotope chronology methods such as U-Pb, K-Ar, and Rb-Sr. However, as a new chronology technique, ⁴⁰Ar/³⁹Ar is rarely used in studying Huangling granite. In this study, the age of amphibole in metamorphic rocks and muscovite and biotite in Huanglingmiao granite has been determined by ⁴⁰Ar/³⁹Ar stage heating technique. The plateau age of amphibole was (835.1±0.8) Ma, and the plateau age of muscovite was (830.0±1.7) Ma. The biotite sample yielded an age spectrum with an upward convex shape, and no obvious flat section was formed. It was concluded that the age of amphibole is much lower than the formation age and metamorphic age of metamorphic rocks, but slightly higher than the muscovite age of nearby granite, indicating the time when the surrounding rock was reset by granite baking and then cooled to 500 ℃. The muscovite age indicates the time Huangling granite cooled to 350 ℃. Both of them restrict the formation time of Huangling granite. Although no plateau age was obtained, the biotite sample gave a meaningful age of 216 Ma in the low-temperature steps, which probably indicates the occurrence time of thermal disturbance in the later stage. The collision and merging of the North China and Yangtze plates caused the slow uplift of the Huangling, and activity of the NNW-trending faults in the Huangling area, and caused the thermal effect enough to affect the Ar closure of the biotite. The high precision ⁴⁰Ar/³⁹Ar age provides accurate chronological support for determining the tectonic evolution history of Huangling granite.
- Huangling Granite,
- Huangling Uplift,
- ⁴⁰Ar/³⁹Ar dating,
- thermal events,
- geochemistry

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References(66)

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40Ar/39Ar Ages of Gneiss and Granite from Huangling Uplift and Their Tectonic Significance

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⁴⁰Ar/³⁹Ar Ages of Gneiss and Granite from Huangling Uplift and Their Tectonic Significance