黑龙江省东部晚三叠世-中侏罗世硅质岩地球化学特征及形成环境

doi:10.13686/j.cnki.dzyzy.2021.06.001

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Abstract The Nadanhada accretionary complex in eastern Heilongjiang Province is mainly composed of the Late Triassic-Middle Jurassic radiolarian siliceous rocks intercalated with the mafic-ultramafic complex and Late Paleozoic shallow sea sedimentary rocks. The analysis results of siliceous rocks from Shichang, Qindeli and Shengli Farm areas in eastern Heilongjiang Province show that the samples, characterized by generally low Al₂O₃, TiO₂, CaO and ΣREE contents and low Al₂O₃/(Al₂O₃+TFe₂O₃) ratio and high SiO₂ content, are pure siliceous rocks. Combined with the Al-Fe-Mn triangle diagram and K₂O/Na₂O ratio, it is indicated that the formation of siliceous rocks has nothing to do with seafloor hydrothermal process. The element discrimination diagram and geochemical characteristics reveal the siliceous rocks in the above three areas were formed in continental slope and marginal sea environment.

Key words： siliceous rock Late Triassic-Middle Jurassic geochemical characteristic formation environment Heilongjiang Province

Received: 08 May 2019

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P595

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	SUN Lei
	ZENG Zhen
	CUI Wei-long
	WANG Xiao-jie
	ZHAO Qing-nian
	HAO Zhen-qun
	LI Han
	ZHANG Hong-ze
	ZHOU Jiang

Cite this article:

SUN Lei,ZENG Zhen,CUI Wei-long等. GEOCHEMISTRY AND FORMATION ENVIRONMENT OF THE LATE TRIASSIC-MIDDLE JURASSIC SILICEOUS ROCKS IN EASTERN HEILONGJIANG PROVINCE[J]. GEOLOGY AND RESOURCES, 2021, 30(6): 637-645.

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http://manu25.magtech.com.cn/Jweb_dzyzy/EN/10.13686/j.cnki.dzyzy.2021.06.001 OR http://manu25.magtech.com.cn/Jweb_dzyzy/EN/Y2021/V30/I6/637

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