Lower crustal contribution to the magma formation of the Damiao massif type anorthosite, North China Craton: Evidence from zircon Hf-O isotopes
文献类型：期刊论文
| 作者 | He, Hai-Long1,2; Song, Xie-Yan2; Zhai, Ming-Guo1,3; Yu, Song-Yue2; Du, Zhi-Song4 |
| 刊名 | PRECAMBRIAN RESEARCH
 |
| 出版日期 | 2019-09-15 |
| 卷号 | 332页码:14 |
| 关键词 | Anorthosite Damiao Massif-type anorthosite Zircon Hf-O isotopes Earth's Middle Age Anorogenic |
| ISSN号 | 0301-9268 |
| DOI | 10.1016/j.precamres.2019.105396 |
| 英文摘要 | The formation of massif-type anorthosites and the associated mangerite, chamockite and (rapakivi-) granite (AMCG suite) are mostly restricted in the "Earth's Middle Age" (similar to 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 similar to 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 delta O-18 values (5.1-7.4) and ancient crustal-like epsilon(Hf)(T) values (-4.0 to -8.9). Since the significant Lu-177/Hf-176 reduction in the lower mafic crust, the mafic lower crustal materials derived from depleted mantle could display an ancient crustal medium to high negative epsilon(Hf)(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 delta O-18 features. Thus, the decoupling of mantle-like delta O-18 and ancient crustal-like epsilon(Hf)(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 epsilon(Hf)(T), initial Sr-87/Sr-86 and 8180 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 (similar to 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. |
| WOS关键词 | MAFIC DYKE SWARMS ; U-PB AGES ; KOROSTEN AMCG COMPLEX ; CENTRAL OROGENIC BELT ; RAPAKIVI GRANITE ; GRENVILLE-PROVINCE ; IN-SITU ; LU-HF ; PROTEROZOIC ANORTHOSITE ; GEOLOGICAL SIGNIFICANCE |
| 资助项目 | National Natural Science Foundation of China[41630316] ; National Natural Science Foundation of China[41873026] ; National Key Research and Development Program of China[2016YFC0600502] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000487566500011 |
| 出版者 | ELSEVIER |
| 资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/93701]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
| 通讯作者 | Song, Xie-Yan; Zhai, Ming-Guo |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, 19 Beitucheng West Rd, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, 99 Lincheng West Rd, Guiyang 550002, Guizhou, Peoples R China 3.Univ Chinese Acad Sci, Key Lab Computat Geodynam, Beijing 100049, Peoples R China 4.4th Geol Team Hebei Geol & Min Bur, Chengde 067000, Peoples R China |
| 推荐引用方式 GB/T 7714 | He, Hai-Long,Song, Xie-Yan,Zhai, Ming-Guo,et al. 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,2019,332:14. |
| APA | He, Hai-Long,Song, Xie-Yan,Zhai, Ming-Guo,Yu, Song-Yue,&Du, Zhi-Song.(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,332,14. |
| MLA | He, Hai-Long,et al."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):14. |
入库方式： OAI收割
来源：地质与地球物理研究所
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