后碰撞阶段的“俯冲型”岩浆岩:来自东昆仑瑙木浑沟晚三叠世闪长玢岩的证据

张明东; 马昌前; 王连训; 郝峰华; 郑少杰; 张磊

doi:10.3799/dqkx.2018.715

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 1183-1206

Zhang Mingdong, Ma Changqian, Wang Lianxun, Hao Fenghua, Zheng Shaojie, Zhang Lei, 2018. Subduction-Type Magmatic Rocks in Post-Collision Stage: Evidence from Late Triassic Diorite-Porphyrite of Naomuhungou Area, East Kunlun Orogen. Earth Science, 43(4): 1183-1206. doi: 10.3799/dqkx.2018.715

Citation:

Zhang Mingdong, Ma Changqian, Wang Lianxun, Hao Fenghua, Zheng Shaojie, Zhang Lei, 2018. Subduction-Type Magmatic Rocks in Post-Collision Stage: Evidence from Late Triassic Diorite-Porphyrite of Naomuhungou Area, East Kunlun Orogen. Earth Science, 43(4): 1183-1206. doi: 10.3799/dqkx.2018.715

Citation:

Zhang Mingdong, Ma Changqian, Wang Lianxun, Hao Fenghua, Zheng Shaojie, Zhang Lei, 2018. Subduction-Type Magmatic Rocks in Post-Collision Stage: Evidence from Late Triassic Diorite-Porphyrite of Naomuhungou Area, East Kunlun Orogen. Earth Science, 43(4): 1183-1206. doi: 10.3799/dqkx.2018.715

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Subduction-Type Magmatic Rocks in Post-Collision Stage: Evidence from Late Triassic Diorite-Porphyrite of Naomuhungou Area, East Kunlun Orogen

doi: 10.3799/dqkx.2018.715

1.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2017-12-20
Publish Date: 2018-04-15

Abstract

Abstract

The East Kunlun orogenic belt in the northeast of Qinghai-Tibet plateau contains large-scale crust-mantle mixed granitoid in the Late Permian and Late Triassic periods. It is an ideal region to investigate crust-mantle mixing and continental crust growth-recycling.In this paper, detailed petrography, LA-ICP-MS zircon U-Pb isotopic geochronology, mineral chemistry, rock geochemistry and Sr-Nd isotopes from the Naomuhungou diorite-porphyrites are reported. Zircon U-Pb ages indicate that the diorite-porphyrites were emplaced at~215.4±3.6 Ma.Plagioclase phenocrysts mainly comprise andesine and a small amount of labradorite, characterized by normal zoning and reverse zoning texture. Amphibole phenocrysts belong to the endenite. Naomuhungou diorite-porphyrites are characterized by the metaluminous to peraluminous, relatively rich in magnesium (Mg^#~51.2) and middle K-high K calc-alkaline. The rock samples display marked enrichment in LREE and LILE (e. g. Rb, Th, U and K), and depleted in some HREE and HFSE (e.g., Nb, Ta, Ti), showing affinities similar to continental arc granites. In addition, the rocks have a homogeneous I_Sr value (0.708 6-0.708 8) and relatively low ε_Nd(t) ((-5.3)-(-4.8)), and have a relatively older model age of T_DM2 (1.38-1.43 Ga). The above mineralogical and geochemical characteristics suggest that diorite-porphyrite might originate from the enriched mantle-derived magmatic underplating of the ancient basement crust and homogeneous mixing with crustal melts, with obvious MASH features. In combination with regional geology studies, it is concluded that the Naomuhungou diorite-porphyrites may have formed during the transitional period of Late A'nemaqen Paleo-Tethys ocean subduction and collision with the continent, and may represent the post-magmatic-response to the suturing of the Bayan Har-Songpan-Ganzi-East Kunlun terrane.This study is also helpful for understanding the origin of the continental crustal accretion through magmatism in the broad context of orogenesis from seafloor subduction to continental collision and to post-collisional processes.
- East Kunlun,
- Naomuhungou,
- geochronology,
- geochemistry,
- diorite-porphyrite,
- Late Triassic,
- magma mixing

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References(131)

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