官道口群凝灰岩SHRIMP锆石U-Pb年龄及华北克拉通中-新元古界地层格架探讨-岩石矿物学杂志-CSCIED科技核心评价数据库-手机版

官道口群凝灰岩SHRIMP锆石U-Pb年龄及华北克拉通中-新元古界地层格架探讨

SHRIMP zircon U-Pb dating of tuff in the Guandaokou Group: Implications for the Meso-Neoproterozoic chronostratigraphic framework of the North China Craton

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DOI	10.20086/j.cnki.yskw.2025.4111
刊名	岩石矿物学杂志 Acta Petrologica et Mineralogica
年，卷(期)	2025, 44(4)
作者	张恒，周洪瑞，丁孝忠，张传恒，高林志*，宋彪,
作者单位	1. 中国地质科学院地质研究所, 北京 100037; 2. 中国地质大学(北京), 北京 100083
摘要	近年来,中国中-新元古界年代地层研究取得了系列进展,为建立我国中-新元古界标准地层提供了可靠数据和候选剖面。本文进一步补充华北克拉通南缘中元古界年代地层研究新进展,包括: 在陕西洛南县和岐山县龙家园组凝灰岩夹层中分别获得1 526±16 Ma(MSWD=0.43, n=8)和1 535±11 Ma(MSWD=0.68, n=12)的SHRIMP锆石U-Pb年龄,进一步验证和约束了龙家园组的时代; 对杜关组凝灰质粉砂岩夹层进行SHRIMP锆石U-Pb年龄研究,限定了杜关组的时代老于1 385±46 Ma(MSWD=1.07, n=6)。这些年龄数据进一步将官道口群归属为蓟县系,从而为华北北缘和南缘的蓟县系进行对比研究提供了锚点。结合前人研究成果,本文尝试建立了华北克拉通中-新元古界年代地层格架,进而为填补待建系和建立青白口系标准剖面提供了备选地层实体。华北南缘洛峪口组、龙家园组、杜关组等获得精确凝灰岩锆石U-Pb年龄,完善了华北克拉通长城系、蓟县系的地层对比方案。长城系、蓟县系在华北地区可以完整连续的建立起来,成为这个时代标准地层的有力备选,但是,华北克拉通待建系和青白口系出露零散、连续性差,同时难以寻找到精确标定地层时代的测年对象,短期很难填补地层柱中的缺失地层(1.3~0.8 Ga),很难在华北地区建立待建系和青白口系标准剖面。
Abstract	Recent advances in Meso-Neoproterozoic chronostratigraphic research in China have yielded critical datasets and candidate sections for establishing standardized stratigraphic frameworks. This study presents new chronostratigraphic findings from the southern margin of the North China Craton. Zircon U-Pb dating reveals that tuff interbeds in the Longjiayuan Formation from Luonan County (1 526±16 Ma, MSWD=0.43, n= 8) and Qishan County (1 535±11 Ma, MSWD=0.68, n=12), Shaanxi Province, constrain these deposits to ca. 1.53~1.52 Ga. SHRIMP U-Pb ages of tuffaceous siltstone interbeds in the Duguan Formation further indicate an age older than 1 385±46 Ma (MSWD=1.07, n= 6). Integrating these results with prior studies, we propose a revised Mesoproterozoic chronostratigraphic framework for North China, addressing the stratigraphic void within the Unnamed System and advancing the standardization of the Qingbaikou System. High-precision tuff-zircon ages from the Luoyukou Formation, Longjiayuan Formation, and Duguan Formation enhance regional correlations between the Changcheng System and Jixian System, supporting their establishment as continuous, complete stratigraphic units and strong candidates for global geostratigraphic standards. Nevertheless, the discontinuous distribution of the Unnamed System and Qingbaikou System in North China, coupled with insufficient geochronological constraints, presents challenges for reconstructing the 1.3~0.8 Ga stratigraphic column and formalizing these systems as standardized geostratigraphic units in the near term.
关键词	华北克拉通；中-新元古界；龙家园组；杜关组；锆石U-Pb年龄
KeyWord	the North China Craton; Meso-Neoproterozoic; the Longjiayuan Formation; the Duguan Formation; zircon U-Pb dating
基金项目
页码	745-766

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张恒，周洪瑞，丁孝忠，张传恒，高林志*，宋彪. 官道口群凝灰岩SHRIMP锆石U-Pb年龄及华北克拉通中-新元古界地层格架探讨 [J]. 岩石矿物学杂志. 2025; 44; (4). 745 - 766.

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