Contrasting Late Carboniferous and Late Permian-Middle Triassic intrusive suites from the northern margin of the North China craton: Geochronology, petrogenesis, and tectonic implications
文献类型：期刊论文
| 作者 | Zhang, Shuan-Hong1,2; Zhao, Yue1; Song, Biao2; Hu, Jian-Min1; Liu, Shu-Wen3; Yang, Yue-Heng4; Chen, Fu-Kun4; Liu, Xiao-Ming5; Liu, Jian1 |
| 刊名 | GEOLOGICAL SOCIETY OF AMERICA BULLETIN
 |
| 出版日期 | 2009 |
| 卷号 | 121期号:1-2页码:181-200 |
| 关键词 | North China craton late Paleozoic-early Mesozoic active continental margin petrogenesis Sr-Nd-Hf isotopes Central Asian orogenic system |
| ISSN号 | 0016-7606 |
| DOI | 10.1130/B26157.1 |
| 文献子类 | Review |
| 英文摘要 | Two contrasting intrusive suites have been identified from the northern margin of the North China craton: a Late Carboniferous diorite-granodiorite suite mainly made up of quartz diorite, diorite, granodiorite, tonalite, and hornblende gabbro, and a Late Permian-Middle Triassic suite of granitoid intrusions consisting of monzogranite, syenogranite, and quartz, monzonite. Plutons from the Late Carboniferous suite exhibit variable SiO(2) contents and calc-alkaline or high-K calc-alkaline, metaluminous geochemical features. Most have low negative whole-rock epsilon(Nd)(T) values (where T is the crystallization age) of -17.1 to -11.5 and zircon epsilon(Hf)(T) values of -38.3 to -11.2, indicating that they were derived mainly from anatectic melting of the ancient lower crust with some involvement of mantle materials. However, an older pluton in the suite exhibits higher epsilon(Nd)(T) values of -11.5 to -9.9, Nd model ages of 1.82-1.64 Ga, lower initial (87)Sr/(86)Sr ratios of 0.7046-0.7048, and it contains some zircon grains that are characterized by high negative to positive zircon epsilon(Hf)(T) values of -8.7 to 1.2, indicating strong involvement of juvenile materials derived from the lithospheric mantle. The Late Carboniferous plutons are interpreted as subduction-related and to have been emplaced in an Andean-style continental-margin arc during the southward subduction of the paleo-Asian oceanic plate beneath the North China craton. Rocks from the Late Permian-Middle Triassic intrusive suite display geochemical signatures ranging from highly fractionated I-type to A-type. They exhibit higher zircon cur(T) values of -14.9 to -6.7, whole-rock epsilon(Nd)(T) values of -10.6 to -8.8, and younger Hf and Nd model ages than most of the Late Carboniferous plutons, indicating that they could have been produced by extreme fractional crystallization of hybrid magmas resulted from mixing of coeval mantle- and crust-derived melts. They are interpreted as postcollisional/ postorogenic granitoids linked to lithospheric extension and asthenosphere upwelling due to slab break-off and subsequent sinking after final collision and suturing of the Mongolian arc terranes with the North China craton. These two contrasting intrusive suites suggest that the final closure of the paleo-Asian Ocean and collision between the Mongolian arc terranes and the North China craton occurred during the Late Permian, and these events were followed by postcollisional/ postorogenic extension, large-volume magmatism, and significant continental growth. No significant syncollisional crustal thickening, high-pressure metamorphism, or S-type granitoid magmatism occurred during the collision process. |
| WOS关键词 | ASIAN OROGENIC BELT ; U-PB GEOCHRONOLOGY ; ND ISOTOPIC CHARACTERISTICS ; CRUST-MANTLE INTERACTION ; WESTERN UNITED-STATES ; INNER-MONGOLIA ; HEBEI PROVINCE ; THRUST BELT ; GEOCHEMICAL CHARACTERISTICS ; EXPERIMENTAL CONSTRAINTS |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000262409800012 |
| 出版者 | GEOLOGICAL SOC AMER, INC |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/71526]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Zhang, Shuan-Hong |
| 作者单位 | 1.Chinese Acad Geol Sci, Inst Geomechan, Key Lab Crustal Deformat & Proc, Beijing 100081, Peoples R China 2.Chinese Acad Geol Sci, Beijing SHRIMP Ctr, Beijing 100037, Peoples R China 3.Peking Univ, Sch Earth & Space Sci, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 5.NW Univ Xian, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang, Shuan-Hong,Zhao, Yue,Song, Biao,et al. Contrasting Late Carboniferous and Late Permian-Middle Triassic intrusive suites from the northern margin of the North China craton: Geochronology, petrogenesis, and tectonic implications[J]. GEOLOGICAL SOCIETY OF AMERICA BULLETIN,2009,121(1-2):181-200. |
| APA | Zhang, Shuan-Hong.,Zhao, Yue.,Song, Biao.,Hu, Jian-Min.,Liu, Shu-Wen.,...&Liu, Jian.(2009).Contrasting Late Carboniferous and Late Permian-Middle Triassic intrusive suites from the northern margin of the North China craton: Geochronology, petrogenesis, and tectonic implications.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,121(1-2),181-200. |
| MLA | Zhang, Shuan-Hong,et al."Contrasting Late Carboniferous and Late Permian-Middle Triassic intrusive suites from the northern margin of the North China craton: Geochronology, petrogenesis, and tectonic implications".GEOLOGICAL SOCIETY OF AMERICA BULLETIN 121.1-2(2009):181-200. |
入库方式： OAI收割
来源：地质与地球物理研究所
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