饶河杂岩中枕状玄武岩的锆石U－Pb年代学、地球化学及其地质意义

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Abstract As one of the most reliable geological records of paleo-Pacific Plate subduction in eastern China, the Nadanhada accretionary complex is of great importance to define the westward subduction of paleo-oceanic plate. The Raohe Complex is located in the core of the complex, developed with typical accretionary complex association, among which the basaltoids, mostly in structural lenticles, are occurred in the ultramafic-mafic complex zone with slight deformation but no metamorphism. Study on the isotopic chronology and geochemistry of the pillow basalt samples from Raohe Complex shows that the LA-ICP-MS zircon U-Pb age is Middle Jurassic(168±2 Ma), with depletion of LILEs (Rb and Sr), enrichment of HFSEs(Nb and Ta) and high-abundant Th, which was formed in the ocean island environment (OIB). Its formation age and genetic environment is significant to study the tectonic dynamic background of the area during the Jurassic period.

Key words： Raohe Complex pillow basalt zircon U-Pb chronology geochemistry Heilongjiang Province

Received: 30 May 2018

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	ZENG Zhen
	SUN Lei
	ZHANG Xing-zhou
	CUI Wei-long
	JIANG Li

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ZENG Zhen,SUN Lei,ZHANG Xing-zhou等. ZIRCON U-Pb CHRONOLOGY AND GEOCHEMISTRY OF THE PILLOW BASALTS FROM RAOHE COMPLEX: Geological Implications[J]. GEOLOGY AND RESOURCES, 2019, 28(2): 119-127.

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http://manu25.magtech.com.cn/Jweb_dzyzy/EN/ OR http://manu25.magtech.com.cn/Jweb_dzyzy/EN/Y2019/V28/I2/119

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