黑龙江省太平岭地区下二叠统双桥子组岩石地球化学特征及其成矿意义

何谋惷; 丁振举; 魏连喜; 周腾飞

doi:10.3799/dqkx.2020.105

Volume 46 Issue 5

May 2021

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He Mouchun, Ding Zhenju, Wei Lianxi, Zhou Tengfei, 2021. Geochemical Characteristics and Metallogenic Significance of Lower Permian Shuangqiaozi Formation in Taiping Mountains, Heilongjiang Province. Earth Science, 46(5): 1537-1553. doi: 10.3799/dqkx.2020.105

Citation:

He Mouchun, Ding Zhenju, Wei Lianxi, Zhou Tengfei, 2021. Geochemical Characteristics and Metallogenic Significance of Lower Permian Shuangqiaozi Formation in Taiping Mountains, Heilongjiang Province. Earth Science, 46(5): 1537-1553. doi: 10.3799/dqkx.2020.105

Citation:

He Mouchun, Ding Zhenju, Wei Lianxi, Zhou Tengfei, 2021. Geochemical Characteristics and Metallogenic Significance of Lower Permian Shuangqiaozi Formation in Taiping Mountains, Heilongjiang Province. Earth Science, 46(5): 1537-1553. doi: 10.3799/dqkx.2020.105

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Geochemical Characteristics and Metallogenic Significance of Lower Permian Shuangqiaozi Formation in Taiping Mountains, Heilongjiang Province

doi: 10.3799/dqkx.2020.105

He Mouchun^{1, 2
,
,},
Ding Zhenju^{1, 2
,
,},
Wei Lianxi^{3
,
,},
Zhou Tengfei³

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
National Demonstration Center for Experimental Mineral Exploration Education, China University of Geosciences, Wuhan 430074, China
3.
Non-Ferrous Metals of Geological Survey and Research Institute of Heilongjiang Province, Harbin 150090, China

Received Date: 2020-10-05
Publish Date: 2021-05-15

Abstract

Abstract

The metallogenic belt in the Taiping Mountains is one of the most important copper-gold polymetallic metallogenic belts in Heilongjiang Province,in which mesothermal hydrothermal vein dominates,followed by porphyry,epithermal and magmatic type deposits. The Lower Permian Shuangqiaozi Formation (P₁s) is widely developed in this region,and is composed of pelite,siltstone,and sandstone,with multiple layers of intermediate-felsic volcanic rocks. The contents of Au,P,and Fe are relatively high in this stratum. In recent years,small scale gold deposits such as Lujiaoling,Wudaogou-23 Gongli have been found in Dongning County and Muleng City. The gold ore bodies are developed in P₁s as veins,but the grade of gold is low,which directly affects the next step of exploration. Based on field investigations,in this paper it uses rock geochemistry,X-ray powder diffraction,and organic carbon analysis to determine the rock types,sedimentary sources,and sources of ore-forming elements such as Au. The contents of major elements display small variations. Compared with PAAS,the rocks are slightly depleted in Al₂O₃,P₂O₅,CaO,and MnO₂,and moderately depleted in Na₂O,MgO,TiO₂,and Fe₂O₃. All trace elements except Zn yield lower contents. The total amount of rare earth elements is equivalent to that of North American shale,and the differentiation of light and heavy rare earth elements is slightly lower than that of North American shale. The rocks are dominated by clay minerals (illite,chlorite) and quartz,with various amounts of albite and minor carbonate minerals and pyrite. The TOC contents of the rock range from 0.22% to 2.52%,with an average of 1.10%. There is no correlation between the contents of Au and TOC and clay minerals. It is suggested that P₁s in the area is composed of carbonaceous slate,and the sediments were mainly derived from the weathering products of quartzose sedimentary rocks,with a small amount derived from femic igneous rocks. The deposition environment is near-shore. The high contents of gold in the stratum were not brought by the fluids after diagenesis and adsorbed by the rich organic compounds or clay minerals,but derived from terrigenous weathering products. This indicates that the gold deposits developed in P₁s in this area are not stratabound gold deposits,but hydrothermal vein type deposits controlled by faults.
- carbonaceous slate,
- Shuangqiaozi Formation,
- sediment provenance,
- metallogenic belt in the Taiping Mountains,
- Heilongjiang Province,
- mineral deposit

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References(55)

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