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Mineralization time and tectonic setting of the Zhengguang Au deposit in the Duobaoshan ore field, Heilongjiang Province, NE China

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Abstract

The Zhengguang deposit, a representative large gold deposit in the Duobaoshan ore field in NE China, is located in the northeast of the Central Asian Orogenic Belt (CAOB). Ore body emplacement was structurally controlled and occurs mainly at the contact zone between the strata of Duobaoshan Formation and an Ordovician diorite stock. The diorite rocks have a close genetic relationship with Au mineralization. Re–Os isotope dating of Au-bearing pyrite yields an isochron age of 506 ± 44 Ma (MSWD = 15). Based on present and previous dating results, it can be concluded that the Zhengguang deposit formed at ~480 Ma. The mineralization time of the Zhengguang deposit is nearly identical to those of the Duobaoshan and Tongshan deposits, indicating they are all derived from the same metallogenic system. The Duobaoshan-style porphyry Cu–Mo mineralization may exist at deeper levels at Zhengguang. The geochemical characteristics of the Zhengguang dioritic rocks presented in this paper are similar to those of bajaitic high-Mg andesite, and the magmas originated from a mantle wedge metasomatized by melts from a subducting oceanic slab at an active continental margin setting. The Ordovician magmatic–metallogenic events in the Duobaoshan ore field were caused by the westward subduction of an oceanic slab located between the Xing’an and Songliao blocks. It is worth pointing out that the Zhengguang deposit is the oldest known Phanerozoic Au deposit in NE China. Further studies of this deposit will improve understanding of the regularity of ore formation and aid mineralization forecast across the Duobaoshan region.

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Acknowledgments

This work was supported by the National Basic Research Program of China (also called 973 Program) (2013CB429802). Thanks are also due to the Heilongjiang Heilong Mining Formation Co., Ltd., Harbin, China. We are grateful to the Re-Os Laboratory of National Research Center of Geoanalysis (CAGS) and Laboratory of Mineralization and Dynamics (Chang’an University).

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Authors and Affiliations

  1. College of Earth Sciences, Jilin University, 2199 Jianshe Street, Changchun, 130061, China

    Yu-Jie Hao, Yun-Sheng Ren, Xuan Zhao & Qun Yang

  2. No.3 Gold Geological Party of CAPF, Harbin, 150086, China

    Ming-Xin Duan

  3. Heilongjiang Heilong Mining Group Co., Ltd, Harbin, 150090, China

    Kuang-Yin Tong

  4. National Research Center for Geoanalysis, Beijing, 100037, China

    Chao Li

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  1. Yu-Jie Hao
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  4. Xuan Zhao
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Correspondence to Yun-Sheng Ren.

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Hao, YJ., Ren, YS., Duan, MX. et al. Mineralization time and tectonic setting of the Zhengguang Au deposit in the Duobaoshan ore field, Heilongjiang Province, NE China. Arab J Geosci 9, 655 (2016). https://doi.org/10.1007/s12517-016-2666-5

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