Nanhuan-Sinian Sedimentary Strata Correlation and Its Provenance Feature in Southeastern Part of South China Block: Implications for Tectonic Evolution
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摘要: 华南板块东南部南华纪‒震旦纪的沉积大地构造背景等问题尚存在争议，本文以研究区内北东‒南西向分布、砂岩‒板岩夹砾岩为主要特征的碎屑岩地层为突破口，开展区域地层对比及物源示踪，进而对该地区沉积大地构造背景进行约束.对闽西南、赣中、湘东南以及桂北4个地区的代表性南华纪‒震旦纪沉积地层剖面开展了岩性对比和碎屑锆石定年工作，结果显示：研究区内不同地区南华纪‒震旦纪碎屑岩地层的岩石组合及沉积序列特征相似，以900~1 100 Ma年龄峰值为特征的物源从南华纪早期至震旦纪持续地从南东向北西推进.同时，本文从岩性和物源两个方面定义了“华夏型陆源碎屑地层”.研究结果对政和‒大埔断裂带以西的扬子陆块和华夏地块之间在南华纪‒震旦纪存在宽阔大洋的分隔提出了质疑.Abstract: The sedimentary tectonic background of the southeastern part of South China Block (SCB) remains controversial. This study focuses on the set of NE-SW stretching clastic sedimentary with alternating lithology of sand and slate with regional gravel interbeds, conducting the sedimentary strata correlation and detrital zircon U-Pb ages in order to constrain the sedimentary tectonic background. Four Nanhuan-Sinian sedimentary strata sections have been studied and the results show that Nanhuan-Sinian sedimentary of the southeastern part of SCB could be well correlated and provenance with detrital zircon age peak of 900-1 100 Ma migrated from southeast to northwest from the Early Nanhuan to Sinian. "Cathaysia-derived Clastic Strata" are identified according to the lithology and provenance features. The results challenge the opinions that there had been a wide ocean between the blocks of Yangtze and Cathaysia during Nanhuan-Sinian to the west of Zhenghe-Dapu Fault in study area.
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Key words:
- South China Block /
- Nanhuan /
- Sinian /
- stratigraphy correlation /
- detrital zircon provenance /
- stratigraphy /
- sedimentology
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图 1 研究区大地构造背景及样品位置示意(据Xu et al., 2016修改)
南华盆地位置根据杜秋定等(2021)；南岭中央裂谷盆地位置根据杨明桂等(2012)；采样位置：1.长汀楼子坝；2.新余下坊；3.郴州泗洲山；4.永福牛河
Fig. 1. Geological setting of study area and locations of samples (after Xu et al., 2016)
图 2 研究区南华系‒震旦系地层对比
#.福建省楼子坝组根据本文发表的及近年来部分未发表的碎屑锆石数据属于震旦纪沉积，福建省地质调查研究院(2017)将其置于下震旦统；*.部分关键地质事件目前只被发现分布于扬子陆块；时间框架综合兰中伍(2023)及参考文献
Fig. 2. Stratigraphy correlation of Nanhuan-Sinian in study area
图 3 本文采样点区域地质简图
a. 闽西南长汀楼子坝；b、c. 赣中新余下坊地区；样品坐标点位见正文
Fig. 3. Simplified regional geological maps of the sampling locations
图 4 样品代表性锆石阴极发光(CL)图像、年龄及采样点露头
图中圆圈代表测年位置，单位Ma
Fig. 4. Cathodoluminescence (CL) images and age of representative zircons from the studied samples in this paper and their outcrops of sampling locations
图 5 赣中闽西北地区南华系‒震旦系碎屑锆石U-Pb年龄分布对比
Nh1-3x为南华系下坊组；Z1b为震旦系坝里组；Z1l为震旦系楼子坝组
Fig. 5. Comparison diagram of Nanhuan-Sinian detrital zircon U-Pb ages distribution
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