A STUDY ON THE PETROGENESIS AND TECTONIC SETTING OF THE SIBAN GRANITE MASS IN ZHALANTUN AREA, GREAT KHINGAN

QIN Tao; LI Lin-chuan; TANG Zheng; JIANG Bin; QIAN Chen; SUN Wei; NA Fu-chao; SHI Lu

Volume 23 Issue 3

Jun. 2017

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Article Navigation > Journal of Geomechanics > 2017 > 23(3): 369-381

QIN Tao, LI Lin-chuan, TANG Zheng, et al., 2017. A STUDY ON THE PETROGENESIS AND TECTONIC SETTING OF THE SIBAN GRANITE MASS IN ZHALANTUN AREA, GREAT KHINGAN. Journal of Geomechanics, 23 (3): 369-381.

Citation:

QIN Tao, LI Lin-chuan, TANG Zheng, et al., 2017. A STUDY ON THE PETROGENESIS AND TECTONIC SETTING OF THE SIBAN GRANITE MASS IN ZHALANTUN AREA, GREAT KHINGAN. Journal of Geomechanics, 23 (3): 369-381.

Citation:

QIN Tao, LI Lin-chuan, TANG Zheng, et al., 2017. A STUDY ON THE PETROGENESIS AND TECTONIC SETTING OF THE SIBAN GRANITE MASS IN ZHALANTUN AREA, GREAT KHINGAN. Journal of Geomechanics, 23 (3): 369-381.

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A STUDY ON THE PETROGENESIS AND TECTONIC SETTING OF THE SIBAN GRANITE MASS IN ZHALANTUN AREA, GREAT KHINGAN

1.
College of Earth Sciences, Jilin University, Changchun City, Jilin Province, 130061, China
2.
Shenyang Institute of Geology and Mineral Resources, Shenyang City, Liaoning Province 110034, China

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Received: 2016-11-18
Published: 2017-06-01

Abstract

Abstract

The Siban rock mass in Zhalantun area of Great Khingan is mainly composed of syenogranites and monzonitic granites with fine-grained diorite enclaves developed inside. LA-ICP-MS zircon U-Pb dating results reveal that the crystallization ages of the monzonitic granite and syenogranite in the Siban rock mass are 291±3 Ma and 303±3 Ma respectively, proving that the Siban rock mass emplaced during the late Paleozoic era. The geochemical results of the whole-rock major and trace elements exhibit that the Siban granite yields high SiO₂ (67.9~77.5 wt%), alkaline components (w (Na₂O+K₂O)=7.55~10.79 wt%) and Al₂O₃ (12.05~16.33 wt%). It is also highly enriched with LREE and LILE while with a depletion of HFSE (e.g. Nb, Ta, Ti and P), which is comparable to high K calc-alkalne I-type granite. The existence of fine-grained diorite enclaves and associated basic rocks developed inside the Siban granlte reveals that the Siban granite has the characteristics of magma mixing between mantle and crustal magmas and subsequently underwent the fractional crystallizations of pyroxene, amphibole, Ti-enriched minerals, plagioclase and apatite, which is supported by their geochemical features. Taken all together, the petrologies, geochemistries and petrogenesises indicate that the Siban rock mass is akin to the post-collision granite and formed by mantle-crust interactions under the delamination of lithospheric mantle environment.
- Zhalantun area,
- Siban granite rock mass,
- Late Carboniferous-Early Permian,
- magma mixing,
- post-collision

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References(36)

References

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