Geochronology, geochemistry and geological significance of Late Triassic magmatism in Qingchengzi orefield, Liaoning. | |
Duan XiaoXia1,2; Liu JianMing1; Wang YongBin1,2; Zhou LingLi1,2; Li YongGui3; Li Bin3; Zhang Zhuang1,2; Zhang ZuoLun4 | |
刊名 | ACTA PETROLOGICA SINICA |
2012-02-01 | |
卷号 | 28期号:2页码:595-606 |
关键词 | Zircon U-Pb dating Adakitic intrusions Syn-collisional granite Qingchengzi orefield, Liaoning |
ISSN号 | 1000-0569 |
文献子类 | Article |
英文摘要 | The Qingchengzi orefield which lies in geotectogene of Liaodong rift is an important polymetallic mineral district in northern China for its clustering several large Pb-Zn, Ag and Au deposits. A phase of Late Triassic magmatism, represented by Shuangdinggou biotite monzogranite and Xinling granite, is intimately related to polymetallic mineralization. LA-ICPMS zircon U-Pb age of 224.2 +/- 1. 2Ma was obtained for the Shuangdinggou intrusion. Geochemical data for the Shuangdinggou intrusion reveal SiO2 content of 69. 07% similar to 71. 31%, while K2O accounts for 3. 53% similar to 5. 22% and Na2O for 3. 87% similar to 4. 14%, indicating it belongs to high K calc-alkaline series. Al2O3 content ranges between 12. 46% similar to 14. 48% and A/CNK <1 suggest metaluminous feature. Trace element geochemistry of the biotite monzogranite displays high total REE content and demonstrate strong fractionation between light and heavy REE elements [(La/Yb)(N) = 35.43 similar to 79. 01, LREE/HREE = 23.09 similar to 35. 10] and minor negative Eu anomalies (delta Eu = 0.68 similar to 0. 97). The biotite monzogranite also shows LILE (such as Rb, Th, K, Pb) enrichment and HFSE (including Nb, Ta, P, Ti) depletion, with unusual high Ba and Sr, low Y and Yb abundances manefesting adakitic geochemical signature. Based on above-stated petrological and geochemical data it is inferred that the biotite monzogranitic magma might be derived from the partial melting of a thickened lower crust with prominent garnet and rutile retained in the residual assemblages, and magma mixing is probably involved based on the unusually high Nb/Ta ratio (18.4 similar to 21.2). It is suggested that slab break-off during the process of Yangtze Craton and North China Craton continental deep subduction in Late Triassic may be responsible for the ore-related magmatism. |
WOS关键词 | NORTH CHINA CRATON ; U-PB ; EASTERN CHINA ; SUBDUCTED LITHOSPHERE ; ZIRCON GEOCHRONOLOGY ; LIAODONG PENINSULA ; CONTINENTAL-CRUST ; PORPHYRY COPPER ; FLAT-SLAB ; PETROGENESIS |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | SCIENCE PRESS |
WOS记录号 | WOS:000301991500019 |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/84402] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Duan XiaoXia |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Grad Sch, Beijing 100049, Peoples R China 3.Dandong Qingchengzi Min Co LTD, Dandong 118107, Peoples R China 4.China Railway Resources Explorat Co, Beijing 100039, Peoples R China |
推荐引用方式 GB/T 7714 | Duan XiaoXia,Liu JianMing,Wang YongBin,et al. Geochronology, geochemistry and geological significance of Late Triassic magmatism in Qingchengzi orefield, Liaoning.[J]. ACTA PETROLOGICA SINICA,2012,28(2):595-606. |
APA | Duan XiaoXia.,Liu JianMing.,Wang YongBin.,Zhou LingLi.,Li YongGui.,...&Zhang ZuoLun.(2012).Geochronology, geochemistry and geological significance of Late Triassic magmatism in Qingchengzi orefield, Liaoning..ACTA PETROLOGICA SINICA,28(2),595-606. |
MLA | Duan XiaoXia,et al."Geochronology, geochemistry and geological significance of Late Triassic magmatism in Qingchengzi orefield, Liaoning.".ACTA PETROLOGICA SINICA 28.2(2012):595-606. |
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