Sedimentary evidence for the early Paleoproterozoic tectono-magmatic lull: Detrital zircon provenance of the 2.47-2.17 Ga Langzishan Formation, Liaohe Group, Eastern Block of the North China Craton
文献类型：期刊论文
| 作者 | Wen, Fei1,2,3,4; Tian, Zhonghua1; Liu, Ping-Hua1; Xu, Wang1; Liu, Fulai1; Mitchell, N. Ross4 |
| 刊名 | JOURNAL OF ASIAN EARTH SCIENCES
 |
| 出版日期 | 2021-11-01 |
| 卷号 | 221页码:15 |
| 关键词 | North China Craton Paleoproterozoic Langzishan formation Detrital zircon provenance analysis Tectonic setting |
| ISSN号 | 1367-9120 |
| DOI | 10.1016/j.jseaes.2021.104939 |
| 英文摘要 | As one of the most ancient cratons in Asia, the North China Craton (NCC) provides an opportunity to examine the evolution of the early earth. However, it is poorly known about the tectonic setting of the Eastern Block of the NCC at 2.47-2.17 Ga. In this study, zircon U-Pb dating was conducted to constrain the provenance, depositional age, and depositional environment of the Langzishan Formation in the Liaodong peninsula, to investigate the tectonic setting of the Eastern Block during the earliest Paleoproterozoic. Provenance analysis suggests that the basal sandstones (protolith of quartzite) in the Langzishan Formation were sourced from 3.8 to 2.5 Ga continental crust, while the overlying sandstone and pelite units were sourced exclusively from 2.5 Ga continental crust. The distribution of detrital zircon ages shows that the basal sandstones of the Langzishan Formation were deposited at 2.47-2.2 Ga, during which the tectonic setting changed from an early collisional setting (2.47-2.35 Ga) to a stable continental margin (2.35-2.2 Ga), whereas pelites in the upper layer of the Langzihsan Formation were deposited at 2.2-2.17 Ga, and also experienced a transition in tectonic setting from a passive continental margin to an active continental margin. The Langzishan Formation is believed to be the lowest sedimentary unit in the Eastern Block. The transition of tectonic setting of this formation shows that the Eastern Block probably has undergone the same transition at 2.47-2.17 Ga, from a collisional setting to a passive continental margin, and then to an active continental margin, possibly related to both onset of the 2.3-2.2 Ga Paleoproterozoic tectonomagmatic lull (TML) and its cessation. |
| WOS关键词 | U-PB GEOCHRONOLOGY ; GRADE METAMORPHIC ROCKS ; ANSHAN-BENXI AREA ; JI OROGENIC BELT ; META-MAFIC ROCKS ; LA-ICP-MS ; LIAODONG PENINSULA ; TECTONIC EVOLUTION ; CRUSTAL EVOLUTION ; BACK-ARC |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000709489100001 |
| 出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/103008]  |
| 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 | Tian, Zhonghua |
| 作者单位 | 1.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China 2.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China 3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wen, Fei,Tian, Zhonghua,Liu, Ping-Hua,et al. Sedimentary evidence for the early Paleoproterozoic tectono-magmatic lull: Detrital zircon provenance of the 2.47-2.17 Ga Langzishan Formation, Liaohe Group, Eastern Block of the North China Craton[J]. JOURNAL OF ASIAN EARTH SCIENCES,2021,221:15. |
| APA | Wen, Fei,Tian, Zhonghua,Liu, Ping-Hua,Xu, Wang,Liu, Fulai,&Mitchell, N. Ross.(2021).Sedimentary evidence for the early Paleoproterozoic tectono-magmatic lull: Detrital zircon provenance of the 2.47-2.17 Ga Langzishan Formation, Liaohe Group, Eastern Block of the North China Craton.JOURNAL OF ASIAN EARTH SCIENCES,221,15. |
| MLA | Wen, Fei,et al."Sedimentary evidence for the early Paleoproterozoic tectono-magmatic lull: Detrital zircon provenance of the 2.47-2.17 Ga Langzishan Formation, Liaohe Group, Eastern Block of the North China Craton".JOURNAL OF ASIAN EARTH SCIENCES 221(2021):15. |
入库方式： OAI收割
来源：地质与地球物理研究所
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