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Lower crustal contribution to the magma formation of the Damiao massif-type anorthosite, North China Craton: Evidence from zircon Hf-O isotopes
Hai-Long He;  Xie-Yan Song;  Ming-Guo Zhai;  Song-Yue Yu;   Zhi-Song Du
2019
Source PublicationPrecambrian Research
Volume332Pages:1-14
Abstract

The formation of massif-type anorthosites and the associated mangerite, charnockite and (rapakivi-) granite (AMCG suite) are mostly restricted in the “Earth’s Middle Age” (~1.70–0.75 Ga), and the magma sources of massif-type anorthosites are highly debated between the depleted mantle and the mafic lower crust. The ~1.7 Ga Damiao massif-type anorthosite in the North China Craton consists mainly of anorthosite and leuconorite with minor melanorite, mangerite, Fe-Ti-(P) ores and abundant ferrodioritic or gabbroic dykes. In-situ zircon Hf-O isotopic data from anorthosite reveal decoupling of mantle-like δ18O values (5.1–7.4) and ancient crustal-like εHf(T) values (−4.0 to −8.9). Since the significant 177Lu/176Hf reduction in the lower mafic crust, the mafic lower crustal materials derived from depleted mantle could display an ancient crustal medium to high negative εHf(T) values after long period of time (e.g., 0.5–1.0 Ga). In contrast, if no supracrustal materials were added, these mafic crustal materials would retain the mantle δ18O features. Thus, the decoupling of mantle-like δ18O and ancient crustal-like εHf(T) values suggest a lower crustal origin of the Damiao massif-type anorthosite. Compilation of Sr-Nd-O isotopic data of massif-type anorthosites reveal decoupling of εHf(T), initial 87Sr/86Sr and δ18O values, which signifies important lower crustal input in magmas sources of most massif-type anorthosites. We proposed that zircon U-Pb age of the Damiao massif-type anorthosite (~1.70 Ga) and regional age correlation suggest that the anorthosite was emplaced in an intraplate, anorogenic extensional setting after the Paleoproterozoic orogeny had ended.

KeywordAnorthosite damiao Massif-type Anorthosite zircon Hf-o Isotopes earth’s Middle Age anorogenic
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/10512
Collection矿床地球化学国家重点实验室
Affiliation1.State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, PR China
2.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, PR China
3.Key Laboratory of Computation Geodynamics, University of Chinese Academy of Sciences, Beijing 100049, PR China
4.The 4th Geological Team of Hebei Geology and Mining Bureau, Chengde 067000, PR China
Recommended Citation
GB/T 7714
Hai-Long He;Xie-Yan Song;Ming-Guo Zhai;Song-Yue Yu; Zhi-Song Du. Lower crustal contribution to the magma formation of the Damiao massif-type anorthosite, North China Craton: Evidence from zircon Hf-O isotopes[J]. Precambrian Research,2019,332:1-14.
APA Hai-Long He;Xie-Yan Song;Ming-Guo Zhai;Song-Yue Yu; Zhi-Song Du.(2019).Lower crustal contribution to the magma formation of the Damiao massif-type anorthosite, North China Craton: Evidence from zircon Hf-O isotopes.Precambrian Research,332,1-14.
MLA Hai-Long He;Xie-Yan Song;Ming-Guo Zhai;Song-Yue Yu; Zhi-Song Du."Lower crustal contribution to the magma formation of the Damiao massif-type anorthosite, North China Craton: Evidence from zircon Hf-O isotopes".Precambrian Research 332(2019):1-14.
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