辽东半岛丹东地区中生代花岗岩锆石U-Pb年龄、Hf同位素特征及其地质意义

张朋; 赵岩; 寇林林; 沙德铭; 毕中伟; 杨凤超

doi:10.3799/dqkx.2019.129

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3297-3313

Zhang Peng, Zhao Yan, Kou Linlin, Sha Deming, Bi Zhongwei, Yang Fengchao, 2019. Zircon U-Pb Ages, Hf Isotopes and Geological Significance of Mesozoic Granites in Dandong Area, Liaodong Peninsula. Earth Science, 44(10): 3297-3313. doi: 10.3799/dqkx.2019.129

Citation:

Zhang Peng, Zhao Yan, Kou Linlin, Sha Deming, Bi Zhongwei, Yang Fengchao, 2019. Zircon U-Pb Ages, Hf Isotopes and Geological Significance of Mesozoic Granites in Dandong Area, Liaodong Peninsula. Earth Science, 44(10): 3297-3313. doi: 10.3799/dqkx.2019.129

Citation:

Zhang Peng, Zhao Yan, Kou Linlin, Sha Deming, Bi Zhongwei, Yang Fengchao, 2019. Zircon U-Pb Ages, Hf Isotopes and Geological Significance of Mesozoic Granites in Dandong Area, Liaodong Peninsula. Earth Science, 44(10): 3297-3313. doi: 10.3799/dqkx.2019.129

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Zircon U-Pb Ages, Hf Isotopes and Geological Significance of Mesozoic Granites in Dandong Area, Liaodong Peninsula

doi: 10.3799/dqkx.2019.129

Shenyang Geological Survey Center, China Geological Survey, Shenyang 110034, China

Received Date: 2019-05-29
Publish Date: 2019-11-11

Abstract

Abstract

In order to determine the rock types, petrogenic age and tectonic setting of the Mesozoic granites from the Dandong area in Liaodong peninsula, the lithology identification, zircon LA-ICP-MS U-Pb dating, major and trace elements, and Hf isotope data for the Sanguliu, Wulongbei and Dingqishan granites are presented in this paper. The LA-ICP-MS U-Pb ages of the Sanguliu pluton of the porphyritic biotite monzogranite and the medium-coarse grained biotite monzogranite are 137.2±1.2 Ma and 123.2±1.3 Ma. The LA-ICP-MS U-Pb geochronology of the Wulongbei medium-fine grained biotite monzogranite and Dinqishan alkali feldspar granite are 146.8±0.8 Ma and 121.1±1.5 Ma.The results of elemental and isotope geochemistry show that the Sanguliu granodiorite belong to shoshonite series, while the porphyritic biotite monzogranite and the medium-coarse grained biotite monzogranite, the Wulongbei medium-fine grained biotite monzogranite and Dinqishan alkali feldspar granite belong to high potassium Ca-alkaline series. Their aluminum indexes (A/CNK ratios) are all less than 1.1, showing the special feature of I-type granite. The samples of the Sanguliu, Wulongbei and Dingqishan granites are enriched in LREE and LILE, but depleted in HREE and HFSE with minor negative Eu anomalies. The zircon ε_Hf(t) values of the three pluton are from -22.40 to -9.77, T_DM2 are between 2 999 and 1 915 Ma, suggesting that the Sanguliu, Wulongbei and Dingqishan granites were mainly derived from the partial melting of the Paleoproterozoic crustal material. Combined with regional tectonic evolution, it is proposed that the Sanguliu, Wulongbei and Dinqishan rock plutonic diagenetic tectonic environment is the active continental margin, the Wulongbei rock may be formed in the compression tectonic environment and the Sanguliu rock and Dinqishan rock may be formed in the extension tectonic environment, which is closely associated with the subduction of the Paleo-Pacific plate.
- Sanguliu pluton,
- Wulongbei pluton,
- Dinqishan pluton,
- zircon U-Pb,
- geochemistry,
- Dandong area of Liaodong peninsula,
- petrology

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References(86)

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