Destruction of the North China Craton in the Mesozoic
文献类型：期刊论文
| 作者 | Wu, Fu-Yuan1,2; Yang, Jin-Hui1,2; Xu, Yi-Gang3,4; Wilde, Simon A.5; Walker, Richard J.6 |
| 刊名 | ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 47
 |
| 出版日期 | 2019 |
| 卷号 | 47页码:173-+ |
| 关键词 | craton destruction North China Mesozoic oceanic subduction mantle plume |
| ISSN号 | 0084-6597 |
| DOI | 10.1146/annurev-earth-053018-060342 |
| 英文摘要 | The North China Craton (NCC) was originally formed by the amalgamation of the eastern and western blocks along an orogenic belt at similar to 1.9 Ga. After cratonization, the NCC was essentially stable until the Mesozoic, when intense felsic magmatism and related mineralization, deformation, pull-apart basins, and exhumation of the deep crust widely occurred, indicative of destruction or decratonization. Accompanying this destruction was significant removal of the cratonic keel and lithospheric transformation, whereby the thick (similar to 200 km) and refractory Archean lithosphere mantle was replaced by a thin (<80 km) juvenile one. The decratonization of the NCC was driven by flat slab subduction, followed by a rollback of the paleo-Pacific plate during the late Mesozoic. A global synthesis indicates that cratons are mainly destroyed by oceanic subduction, although mantle plumes might also trigger lithospheric thinning through thermal erosion. Widespread crust-derived felsic magmatism and large-scale ductile deformation can be regarded as petrological and structural indicators of craton destruction. A craton, a kind of ancient continental block on Earth, was formed mostly in the early Precambrian (>1.8 Ga). A craton is characterized by a rigid lithospheric root, which provides longevity and stability during its evolutionary history. Some cratons, such as the North China Craton, can be destroyed by losing their stability, manifested by magmatism, deformation, earthquake, etc. |
| WOS关键词 | LITHOSPHERIC MANTLE BENEATH ; SINO-KOREAN CRATON ; CENOZOIC INTRAPLATE BASALTS ; SUBCONTINENTAL LITHOSPHERE ; PERIDOTITE XENOLITHS ; TECTONIC EVOLUTION ; LIAODONG PENINSULA ; WATER-CONTENT ; REFERTILIZATION ; GEOCHEMISTRY |
| WOS研究方向 | Astronomy & Astrophysics ; Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000470274200008 |
| 出版者 | ANNUAL REVIEWS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/92271]  |
| 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 | Wu, Fu-Yuan |
| 作者单位 | 1.Chinese Acad Sci, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Inst Earth Sci, Beijing 100029, Peoples R China 3.Chinese Acad Sci, State Key Lab Isotope Geochem, Guangzhou 510640, Guangdong, Peoples R China 4.Chinese Acad Sci, Inst Earth Sci, Guangzhou Inst Geochem, Guangzhou 510640, Guangdong, Peoples R China 5.Curtin Univ Technol, Inst Geosci Res, Dept Appl Geol, Perth, WA 6845, Australia 6.Univ Maryland, Dept Geol, Isotope Geochem Lab, College Pk, MD 20742 USA |
| 推荐引用方式 GB/T 7714 | Wu, Fu-Yuan,Yang, Jin-Hui,Xu, Yi-Gang,et al. Destruction of the North China Craton in the Mesozoic[J]. ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 47,2019,47:173-+. |
| APA | Wu, Fu-Yuan,Yang, Jin-Hui,Xu, Yi-Gang,Wilde, Simon A.,&Walker, Richard J..(2019).Destruction of the North China Craton in the Mesozoic.ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 47,47,173-+. |
| MLA | Wu, Fu-Yuan,et al."Destruction of the North China Craton in the Mesozoic".ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 47 47(2019):173-+. |
入库方式： OAI收割
来源：地质与地球物理研究所
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