Paleoproterozoic gabbronoritic and granitic magmatism in the northern margin of the North China craton: Evidence of crust-mantle interaction

doi:10.1016/j.precamres.2010.08.015

	Paleoproterozoic gabbronoritic and granitic magmatism in the northern margin of the North China craton: Evidence of crust-mantle interaction
	Peng, Peng 1,2; Guo, Jinghui 1; Zhai, Mingguo 1; Bleeker, Wouter 2
刊名	PRECAMBRIAN RESEARCH
	2010-12-01
卷号	183 期号:3 页码:635-659
关键词	North China craton Paleoproterozoic Gabbronorite Dyke and sill Ultra-high-temperature metamorphism Crust-mantle interaction Ridge subduction
ISSN号	0301-9268
DOI	10.1016/j.precamres.2010.08.015
文献子类	Article
英文摘要	Paleoproterozoic Xuwujia gabbronorites in the northern margin of the North China craton occur as dykes, sills and small plutons intruded into khondalite (aluminous paragneisses, sedimentary protoliths deposited at ca. 2.0-1.95 Ga), and as numerous entrained bodies and fragments of variable scales in the Liangcheng granitoids (ca. 1.93-1.89 Ga). These gabbronoritic dykes are present at all locations where ca. 1.93-1.92 Ga ultra-high-temperature metamorphism is recorded in the khondalite. A gabbronorite sample from the Hongmiaozi dyke gives zircon Pb-207/Pb-206 mean ages of 1954 +/- 6 Ma (core domains) and 1925 +/- 8 Ma (rim domains). These ages, as well as previously reported ages, constrain the age of mafic magmatism to be at ca. 1.96-1.92 Ga (similar to 1.93 Ga). One sample from the Xigou gabbro intruded by the Liangcheng granitoids gives a zircon Pb-207/Pb-206 mean age of 1857 +/- 4 Ma, which is interpreted as the age of a metamorphic overprint. The Xuwujia gabbronorites comprise mainly gabbronorite compositions, as well as some norite, olivine gabbronorite, monzonorite, quartz gabbronorite, and quartz monzonorite. Chemically, they are tholeiitic and can be divided into two groups: a high-Mg group (6.2-22.9 wt.% MgO) and a relatively low-Mg group (2.2-5.7 wt.% MgO). The high-Mg group shows negative Eu-anomalies (Eu/Eu=0.53-0.72), slight light rare earth element enrichment (La/Yb-N = 0.56-1.53), and small negative anomalies in high field-strength elements. The epsilon Nd (t=1.93 Ga) values vary from +0.3 to +2.4. The low-Mg group shows varied Eu-anomalies (Eu/Eu=0.48-1.05), and is enriched in light rare earth elements (La/Yb-N=1.51-11.98). The majority shows negative anomalies in high field-strength elements (e.g., Th, Nb, Zr, and Ti). Initial epsilon Nd (at 1.93 Ga) values for low-Mg gabbronorites vary from -5.0 to 0. The Xuwujia gabbronorites possibly experienced assimilation of crust, and fractional crystallization of initially olivine and hypersthene (the high-Mg group), and then olivine, clinopyroxene, and plagioclase (the low-Mg group). The slightly younger Liangcheng granitoids consist of garnet-bearing granite, granodiorite and quartz-rich granitic compositions. They are intermediate to felsic calc-alkaline rocks, thought to be derived from surrounding metasedimentary crust. Xigou gabbro could represent early cumulates. The granitoids have relatively high-Mg numbers (up to 54), and show some chemical affinities with the gabbronorites, which could have resulted from incorporation of gabbronoritic melts. The occurrence and chemical variations of the Xuwujia gabbronorites and Liangcheng granitoids can be interpreted to have resulted from crust-mantle interaction, with mingling and partial mixing of mantle (gabbronoritic) and crustal (granitic) melts. The Xuwujia gabbronorites originated from a mantle region with high potential temperatures (similar to 1550 degrees C), possibly associated with a plume or more likely a ridge-subduction-related mantle upwelling event. They could have had extremely high primary intrusion temperatures (up to 1400 degrees C). Emplacement of these magmas was likely responsible for the extensive crustal anatexis (Liangcheng granitoids) and the local ultra-high-temperature metamorphism. These sequences may have followed ca. 1.95 Ga continent-continent (arc?) juxtaposition and were themselves followed by significant regional uplift and exhumation in the northern margin of the North China craton. (C) 2010 Elsevier B.V. All rights reserved.
WOS关键词	U-PB GEOCHRONOLOGY ; EARTH-ELEMENT MOBILITY ; CONTINENTAL EVOLUTION ; ZIRCON GEOCHRONOLOGY ; TECTONIC EVOLUTION ; RIDGE SUBDUCTION ; TRACE-ELEMENTS ; ISOTOPIC COMPOSITIONS ; METAMORPHIC EVENTS ; IGNEOUS PROVINCE
WOS研究方向	Geology
语种	英语
出版者	ELSEVIER SCIENCE BV
WOS记录号	WOS:000285233200018
资助机构	National Foundation(40730315 ; National Foundation(40730315 ; National Foundation(40730315 ; National Foundation(40730315 ; 90714003 ; 90714003 ; 90714003 ; 90714003 ; 40721062 ; 40721062 ; 40721062 ; 40721062 ; 40602024) ; 40602024) ; 40602024) ; 40602024) ; National Foundation(40730315 ; National Foundation(40730315 ; National Foundation(40730315 ; National Foundation(40730315 ; 90714003 ; 90714003 ; 90714003 ; 90714003 ; 40721062 ; 40721062 ; 40721062 ; 40721062 ; 40602024) ; 40602024) ; 40602024) ; 40602024) ; National Foundation(40730315 ; National Foundation(40730315 ; National Foundation(40730315 ; National Foundation(40730315 ; 90714003 ; 90714003 ; 90714003 ; 90714003 ; 40721062 ; 40721062 ; 40721062 ; 40721062 ; 40602024) ; 40602024) ; 40602024) ; 40602024) ; National Foundation(40730315 ; National Foundation(40730315 ; National Foundation(40730315 ; National Foundation(40730315 ; 90714003 ; 90714003 ; 90714003 ; 90714003 ; 40721062 ; 40721062 ; 40721062 ; 40721062 ; 40602024) ; 40602024) ; 40602024) ; 40602024)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/72396]
专题	中国科学院地质与地球物理研究所
通讯作者	Peng, Peng
作者单位	1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Geol Survey Canada, Ottawa, ON K1A 0E9, Canada
推荐引用方式 GB/T 7714	Peng, Peng,Guo, Jinghui,Zhai, Mingguo,et al. Paleoproterozoic gabbronoritic and granitic magmatism in the northern margin of the North China craton: Evidence of crust-mantle interaction[J]. PRECAMBRIAN RESEARCH,2010,183(3):635-659.
APA	Peng, Peng,Guo, Jinghui,Zhai, Mingguo,&Bleeker, Wouter.(2010).Paleoproterozoic gabbronoritic and granitic magmatism in the northern margin of the North China craton: Evidence of crust-mantle interaction.PRECAMBRIAN RESEARCH,183(3),635-659.
MLA	Peng, Peng,et al."Paleoproterozoic gabbronoritic and granitic magmatism in the northern margin of the North China craton: Evidence of crust-mantle interaction".PRECAMBRIAN RESEARCH 183.3(2010):635-659.