Genesis of Mesozoic high-Mg dioritic rocks from the eastern North China Craton: Implications for the evolution of continental lithosphere
文献类型：期刊论文
| 作者 | Guo, Jun1,2; Huang, Xiao-Long1,2; He, Peng-Li1; Chen, Lin-Li1; Zhong, Jun-Wei3 |
| 刊名 | AMERICAN MINERALOGIST
 |
| 出版日期 | 2024-01-29 |
| 卷号 | 109期号:1页码:198-214 |
| 关键词 | High-Mg dioritic rocks magmatic processes fluid metasomatism sub-continental lithospheric mantle North China Craton |
| ISSN号 | 0003-004X |
| DOI | 10.2138/am-2022-8755 |
| 英文摘要 | Pre-Cenozoic high-Mg andesites (HMAs) are mostly present in continental interiors, but their genetic relationship with continental lithosphere evolution remains unclear because of uncertainties of their mantle source, magmatic processes, and physicochemical conditions of formation. Early Cretaceous high-Mg dioritic rocks (HMDs, analogs of HMAs) of the Jinling complex in the Luxi area are typical intra-plate intrusions of the eastern North China Craton (NCC) and can be subdivided into two groups (Group-I and -II) on the basis of their petrographic and geochemical features. Group-I HMDs show low SiO2 contents (52.47-56.10 wt%) and Sr/Y (34.5-39.6) and (La/Yb)(N) (10.3-13.6) ratios but high contents of MgO (7.86-9.13 wt%), Y (18.3-20.3 ppm), Yb (1.43-1.47 ppm), and compatible elements (Cr = 407-585 ppm; Ni = 117-216 ppm), classifying as sanukitic rocks. Group-II HMDs are characterized by high SiO2 contents (63.81-64.87 wt%) and Sr/Y (47.1-63.4) and (La/Yb)(N) (16.1-17.5) ratios with low MgO (2.90-3.08 wt%), Y (0.88-1.04 ppm), Yb (0.88-1.04 ppm), and compatible elements (Cr = 201-213 ppm; Ni = 55-57 ppm) contents, belonging to adakitic rocks. Group-I and Group-II HMDs of the Jinling complex are closely related in spatial and temporal distribution, and all have enriched Sr-Nd isotopic compositions and arc-like trace element patterns with abundant hydrous minerals. Therefore, the Jinling HMDs should share a common source of ancient sub-continental lithospheric mantle that was metasomatized by aqueous fluids derived from the subducted Paleo-Pacific slab. The Jinling HMDs were not formed from interaction between slab-derived melts and mantle-wedge peridotites but were instead derived from partial melting of hydrous mantle peridotites in the continental interior of the eastern NCC. The distinctly different petrography, geochemistry, and mineralogy of the two groups of rocks resulted mainly from differing magmatic processes at crustal depths. Thus, Pre-Cenozoic intra-plate HMAs/HMDs are genetically distinct from Cenozoic HMAs that were mostly present in arc settings and generally represent juvenile crust growth. In a way, Archean tonalitic-trondhjemiticgranodioritic rocks (TTG) and sanukitoids, geochemically similar to HMAs/HMDs, could also be derived from interaction between slab-derived melts and mantle-wedge peridotites in arc settings or partial melting of hydrous mantle peridotites in continental interiors, and thus might not always be related with continental crustal growth and the onset of plate subduction. |
| WOS研究方向 | Geochemistry & Geophysics ; Mineralogy |
| 语种 | 英语 |
| WOS记录号 | WOS:001134521600010 |
| 源URL | [http://ir.gig.ac.cn/handle/344008/77382]  |
| 专题 | 同位素地球化学国家重点实验室 |
| 通讯作者 | Huang, Xiao-Long |
| 作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Geochem, CAS Ctr Excellence Deep Earth Sci, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 2.Southern Marine Sci & Engn Guangdong Lab Guangzhou, Guangzhou 511458, Peoples R China 3.Kunming Univ Sci & Technol, Fac Land Resources Engn, Kunming, Yunnan, Peoples R China |
| 推荐引用方式 GB/T 7714 | Guo, Jun,Huang, Xiao-Long,He, Peng-Li,et al. Genesis of Mesozoic high-Mg dioritic rocks from the eastern North China Craton: Implications for the evolution of continental lithosphere[J]. AMERICAN MINERALOGIST,2024,109(1):198-214. |
| APA | Guo, Jun,Huang, Xiao-Long,He, Peng-Li,Chen, Lin-Li,&Zhong, Jun-Wei.(2024).Genesis of Mesozoic high-Mg dioritic rocks from the eastern North China Craton: Implications for the evolution of continental lithosphere.AMERICAN MINERALOGIST,109(1),198-214. |
| MLA | Guo, Jun,et al."Genesis of Mesozoic high-Mg dioritic rocks from the eastern North China Craton: Implications for the evolution of continental lithosphere".AMERICAN MINERALOGIST 109.1(2024):198-214. |
入库方式： OAI收割
来源：广州地球化学研究所
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