首页|华南板块东南部南华纪?震旦纪沉积地层区域对比、物源特征及构造演化

华南板块东南部南华纪?震旦纪沉积地层区域对比、物源特征及构造演化

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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900～1100 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.
Nanhuan-Sinian Sedimentary Strata Correlation and Its Provenance Feature in Southeastern Part of South China Block:Implications for Tectonic Evolution
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 900-1100 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.

South China BlockNanhuanSinianstratigraphy correlationdetrital zircon provenancestratigraphysedimentology

宋芳、何垚砚、牛志军、杨文强、王志宏

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古生物与地质环境演化湖北省重点实验室,湖北武汉 430205

中国地质调查局武汉地质调查中心(中南地质科技创新中心),湖北武汉 430205

华南板块 南华纪 震旦纪 地层对比 碎屑锆石 地层学 沉积学

中国地质调查局地质调查项目中国地质调查局地质调查项目中国地质调查局地质调查项目中国地质调查局地质调查项目国家自然科学金面上项目国家自然科学金面上项目古生物与地质环境演化湖北省重点实验室开放基金项目

DD20240038DD20243437DD20243480DD20230226U224421241772019PEL-202106

2024

10.3799/dqkx.2023.158

地球科学
中国地质大学

地球科学

CSTPCD北大核心
影响因子：1.447
ISSN：1000-2383
年,卷(期)：2024.49(9)
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