塔里木大火成岩省二叠纪碱性煌斑岩的岩石成因和深部地球动力学过程

曹俊; 陈苗苗; 万淑敏; 王慧丽; 易辉; 雷恒聪

doi:10.3799/dqkx.2022.490

Volume 49 Issue 7

Jul. 2024

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Article Navigation > Earth Science > 2024 > 49(7): 2448-2474

Cao Jun, Chen Miaomiao, Wan Shumin, Wang Huili, Yi Hui, Lei Hengcong, 2024. Petrogenesis and Deep Dynamic Processes of Early Permian Alkaline Lamprophyres in Tarim Large Igneous Province, NW China. Earth Science, 49(7): 2448-2474. doi: 10.3799/dqkx.2022.490

Citation:

Cao Jun, Chen Miaomiao, Wan Shumin, Wang Huili, Yi Hui, Lei Hengcong, 2024. Petrogenesis and Deep Dynamic Processes of Early Permian Alkaline Lamprophyres in Tarim Large Igneous Province, NW China. Earth Science, 49(7): 2448-2474. doi: 10.3799/dqkx.2022.490

Citation:

Cao Jun, Chen Miaomiao, Wan Shumin, Wang Huili, Yi Hui, Lei Hengcong, 2024. Petrogenesis and Deep Dynamic Processes of Early Permian Alkaline Lamprophyres in Tarim Large Igneous Province, NW China. Earth Science, 49(7): 2448-2474. doi: 10.3799/dqkx.2022.490

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Petrogenesis and Deep Dynamic Processes of Early Permian Alkaline Lamprophyres in Tarim Large Igneous Province, NW China

doi: 10.3799/dqkx.2022.490

Cao Jun^{1, 2, 3
,
,},
Chen Miaomiao^{1, 3},
Wan Shumin^{1, 3},
Wang Huili^{1, 3},
Yi Hui^{1, 3},
Lei Hengcong^{1, 3}

1.
State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
2.
MOE Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring, Central South University, Changsha 410083, China
3.
School of Earth Sciences, East China University of Technology, Nanchang 330013, China

Received Date: 2022-08-10
Available Online: 2024-08-03
Publish Date: 2024-07-25

Abstract

Abstract

The Tarim Large Igneous Province is characterized by long duration of magmatism, complex rock types and wide distribution of iron-rich alkaline basalts, although the source and petrogenesis of magmatism associated with it remain disputed. Here we chose the Wajilitag alkaline lamprophyres in the northwestern margin of the Tarim Large Igneous Province to precisely determine their emplacement ages, constrain its petrogenesis and discuss the deep dynamic processes involved in the formation of the Tarim Large Igneous Province using LA-ICP-MS zircon U-Pb dating, mineral and whole-rock geochemistry. Zircon U-Pb geochronology indicates that the Wajilitag alkaline lamprophyres formed at 279±1 Ma, belonging to the second phase of Tarim Large Igneous Province magmatism. The lamprophyre is characterized by a panidiomorphic-porphyritic texture imparted by olivine, clinopyroxene, amphibole and biotite set in a groundmass of plagioclase, clinopyroxene, amphibole, biotite and titanomagnetite microcrysts. These rocks have low SiO₂ (43.5%-49.4%), high Fe₂O₃t (9.32%-15.50%), high TiO₂ (2.28%-4.58%), and Mg^# numbers of 43.6-52.9, and are enriched in mantle compatible elements (Ni, Cr). Meanwhile, they also show high Na₂O (2.58%-5.50%) and low K₂O/Na₂O ratios (0.31-0.78), highlighting their sodic characters. Fractionated chondrite normalized REE patterns indicates involvement of an enriched mantle source from within the garnet stability field whereas slightly negative K, Sr, Ti and Zr-Hf anomalies displayed on the primitive mantle normalized multi-element spidergram highlight involvement of a subducted component in the mantle source. Bulk-rock (⁸⁷Sr/⁸⁶Sr)_i (0.704 36-0.705 34), ε_Nd(t)(-1.88-+1.10) and (²⁰⁶Pb/²⁰⁴Pb)_i (17.19-17.89) of the Wajilitag alkaline lamprophyres indicate derivation from a slightly depleted mantle source similar to that of asthenospheric magmas such as OIB. Notably, the δ²⁶Mg values of the Wajilitag alkaline lamprophyres are typically lighter than those of the normal mantle source. The primitive magmas of the Wajilitag alkaline lamprophyres are likely derived from low degrees melting of carbonated eclogite bearing mantle plume, and possibly affected by the plume-lithosphere interaction. Ultimately, our study suggests that plume-subducted altered oceanic slab interaction could make important contributions to the genesis of the Tarim Large Igneous Province.
- alkaline lamprophyre,
- Mg isotope,
- Tarim Large Igneous Province,
- mantle plume,
- subducted altered oceanic slab,
- petrology

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References(146)

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Petrogenesis and Deep Dynamic Processes of Early Permian Alkaline Lamprophyres in Tarim Large Igneous Province, NW China

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