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Journal of Earth Science  > 2025  > Corrected proof
Chuntao Zhao, Jinggui Sun, Jilong Han, Jiansen Li, Dongmei Yu, Jinjun Han, Yugang Li, Jianping Wang. Constraints of magmatism on the Da'anhe skarn Au deposit, central Heilongjiang Province, northeastern China. Journal of Earth Science. doi: 10.1007/s12583-025-0361-8
Citation: Chuntao Zhao, Jinggui Sun, Jilong Han, Jiansen Li, Dongmei Yu, Jinjun Han, Yugang Li, Jianping Wang. Constraints of magmatism on the Da'anhe skarn Au deposit, central Heilongjiang Province, northeastern China. Journal of Earth Science. doi: 10.1007/s12583-025-0361-8
shu

Constraints of magmatism on the Da'anhe skarn Au deposit, central Heilongjiang Province, northeastern China

doi: 10.1007/s12583-025-0361-8

  • a Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining, 810008, China bQinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Xining, 810008, China

  • c College of Earth Science, Jilin University, Changchun 130061, China

  • d Development and Research Center of China Geological Survey, Beijing 100037, China

  • e Hebei Environmental Geology Exploration Institute, Hebei Key Laboratory of Geological Resources and Environment Monitoring and Protection, Shijiazhuang, 050021, China

Funds:

the China Postdoctoral Science Foundation (No. 2023M743306).

This work was supported by the Natural Science Foundation of Qinghai Province (No. 2024-ZJ-984)

the National Natural Science Foundation of China (No. 42202068)

  • Available Online: 25 Aug 2025
    Abstract
  • Au-only skarn deposits are not common in China, and their genesis has not been extensively studied. Many skarn deposits were developed in the Lesser Xing'an Range (LXR) of NE China during the Early Jurassic, among which the Da'anhe deposit is unique as it is an Au-only skarn deposit. However, the key factors controlling Au mineralization with respect to coeval Fe, Cu, and Pb-Zn skarns are poorly understood. To determine the genesis and constraint relationship of magmatism on the Da'anhe deposit, we conducted detailed geology, zircon chronology, Lu-Hf isotope geochemistry, and whole-rock and mineral geochemistry analyses on the Da'anhe system. We have reached the following conclusions: (1) The orebodies formed at the contact zone between gabbroic diorite and the Permian marble of the Tumenling Formation. (2) U-Pb analysis of zircon grains reveals that the gabbroic diorite formed at 183.7~185.8 Ma. (3) The primary magma of gabbroic diorite originated from mantle wedges that were metasomatized by subduction fluids. During ascent, the primary magma may have assimilated minor ancient crustal materials, and then underwent fractional crystallization of olivine, pyroxene and hornblende. (4) Compared with the contemporaneous skarn Fe-, Cu-, and Pb-Zn deposits in the LXR area, the ore-related intrusion at Daanhe are characterized by lower degree of differentiation (DI = 51.28~60.34), lower magmatic oxidation states (ΔFMQ = 0.17, log(fO2) = -15.11), but higher water content (6.80 wt.%), which are considered to be the key factors controlling the formation of the Da'anhe Au-only skarn deposit. However, the greater emplacement depth (4.13 km) affects the mineralization scale of the Da'anhe deposit. This study identified the constraints of magmatic activity on the exploration of skarn Au deposits in the LXR, which benefits the exploration of skarn Au deposits.

     

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