赣东北樟树墩早侏罗世水北组碎屑锆石研究及其地质意义

Study and geological implication of detrital zircons in Shuibei Formation of Early Jurassic in Zhangshudun of northeastern Jiangxi Province

赣东北樟树墩地区早侏罗世盆地处于江南造山带东南缘,揭示盆地沉积物质来源对于认识和探讨周缘早中生代造山事件和古地理格局具有重要意义。对樟树墩早侏罗世盆地开展了岩相学、碎屑锆石U-Pb年代学和Lu-Hf同位素研究。结果表明盆地为类磨拉石建造与内陆湖沼含煤建造,碎屑锆石年龄跨度大(2431~263 Ma),未出现同沉积或准同沉积的碎屑锆石;碎屑锆石年龄呈现极强的早古生代峰值(420~380 Ma,εHf(t)为-10.7^-3.0,TDMC为2.08~1.58 Ga)、弱的新元古代峰值(858~663 Ma,εHf(t)为-18.8^-6.7,TDMC为2.79~2.09 Ga)和晚古生代峰值(370~355 Ma),另有少量早中生代((263±5)Ma)、中—古元古代(2431~1224 Ma)碎屑锆石记录。碎屑锆石年龄和Hf同位素组成与华夏地块西北武夷山地区所出露地质体组成相似,而与扬子东南缘地质体组成存在显著差异,其碎屑物质主要来自陆内西北武夷山地区前寒武纪基底和古生代地质体,少量碎屑物质可能来源于浙西北地区,具有被动型大陆边缘盆地沉积特征。综合区域上早中生代盆地研究成果,认为江南造山带东段景德镇—黄山东南在早—中侏罗世并未整体隆升剥蚀,华南内陆中生代的构造-岩浆活动是其周缘多板块俯冲汇聚的构造响应,晚三叠世—早侏罗世古太平洋板块向东亚大陆的俯冲造成华南东南部隆升,使其开始为内陆盆地提供物源,至早—中侏罗世之交构造体制转换为古太平洋板块的俯冲消减。

The Early Jurassic basin in Zhangshudun of northeastern Jiangxi Province is located in the southeastern part of Jiangnan orogeny,and revealing the basin depositional source is of great importance for understanding and discussing the orogenic events and ancient geography during Early Mesozoic.The research of petrography,detrital zircons U-Pb geochronology,Lu-Hf isotope geochemistry of Early Jurassic clastic rocks was conducted in this paper.The results show that the Early Jurassic Shuibei Formation includes molasse-like deposits and fluviatile-lacustrine facies,and the detrital zircons U-Pb ages are within the wide scope of 2431~263 Ma,with no existence of synsedimentary or pensynsedimentary detrital zircons.The detrital zircons display a very obvious peak age in Early Paleozoic of 420~380 Ma,withεHf(t)values between-10.7 and-3 and TDMC values between 2.08 and 1.58 Ga.The weak peak ages of 370~355 Ma and 858~663 Ma are displayed in Late Paleozoic and Neoproterozoic,respectively,withεHf(t)values of-18.8 to-6.7 and TDMC values of 2.08 to 1.58 Ga.The detrital zircons also contain a few Early Mesozoic(263 Ma)and Paleo-Meso proterozoic(2431~1224 Ma)ages.The detrital zircons ages and Lu-Hf isotope are similar with geological entities in northwestern Wuyi area of Cathaysia Block,while they are obviously different from the ages of the geological body in southeastern Yangtze region.The detrital materials are mainly from Early Cambrian basement and Paleozoic geological body northwestern Wuyi area.While little detrital rocks may come from northwestern Zhejiang with sedimentary characters of passive continental margin.Combined with the comprehensive regional research results of Early Mesozoic basin,the authors conclude that the southeastern Jingdezhen-Huangshan of eastern Jiangnan orogenic belt was not uplifting with erosion in Early and Middle Jurassic,and the Mesozoic structural-magmatic activities in the inland of South China were the tectonic response to the dive and influx of multiplates.The uplift in the southezstern part of South China caused by the subduction of the paleo-pacific plate to the East Asian continent from the Late Triassic to Early Jurassic can provide provenance for the inland basin,and the tectonic constitution at the turn of the Early-Middle Jurassic has been transformed into the subduction of the paleo-pacific plate.