Time constraint on the closing of the Paleo-Asian Ocean in northern Beishan of Inner Mongolia: Evidence from Heihongshan admellite

ZHU Wei; ZHANG Zhengping; SUN Yingshu; CHENG Haifeng; TI Zhenhai; DU Jinli; SU Pengtao; FENG Yipeng; LIANG Guoqing

2019 Vol. 38, No. 11

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ZHU Wei, ZHANG Zhengping, SUN Yingshu, CHENG Haifeng, TI Zhenhai, DU Jinli, SU Pengtao, FENG Yipeng, LIANG Guoqing. Time constraint on the closing of the Paleo-Asian Ocean in northern Beishan of Inner Mongolia: Evidence from Heihongshan admellite[J]. Geological Bulletin of China, 2019, 38(11): 1846-1857.

Citation:

ZHU Wei, ZHANG Zhengping, SUN Yingshu, CHENG Haifeng, TI Zhenhai, DU Jinli, SU Pengtao, FENG Yipeng, LIANG Guoqing. Time constraint on the closing of the Paleo-Asian Ocean in northern Beishan of Inner Mongolia: Evidence from Heihongshan admellite[J]. Geological Bulletin of China, 2019, 38(11): 1846-1857.

Time constraint on the closing of the Paleo-Asian Ocean in northern Beishan of Inner Mongolia: Evidence from Heihongshan admellite

1.
Hebei Institute of Regional Geological Survey, Langfang 065000, Hebei, China
2.
Langfang No. 7 Middle School, Langfang 065000, Hebei, China

Received Date: 23 July 2018

Revised Date: 20 August 2018

Publish Date: 15 November 2019

Abstract

Abstract

The Late Carboniferous admellite in the Heihongshan area is located in the northern part of the Hongshishan-Baiheshan-Pengboshan ophiolite belt. The geochemical characteristics show that the admellite belongs to metaluminous to weakly peralic potassium aluminous calc alkaline series I type granite of high differentiation; its LREE enrichment and LREE and HREE fractionation are obvious, with weak Eu negative anomaly and right-inclined rare earth curve. Trace elements are relatively enriched in Ba, K, Zr and Hf but depleted in Nb, Ti, P and Sr, indicating the characteristics of intrusive rocks related to subduction and formed in the volcanic arc environment before collision. The U-Pb dating of LA-ICP-MS zircon yielded weighted average ²⁰⁶Pb/²³⁸U age of 315.2±2.5Ma. Comprehensive studies show that the Heihongshan area belonged to the volcanic arcs on the active continental margin in the Late Carboniferous epoch, and the Hongshishan-Baiheshan-Pengboshan ophiolite belt suggests that the oceanic basin in Heihongshan area was closed in the Late Carboniferous epoch.
- geochemical characteristics /
- zircon U-Pb dating /
- Late Carboniferous /
- admellite /
- Heihongshan

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References

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