高邮凹陷戴南组稀土元素和锆石U-Pb年代特征及构造意义
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摘要
通过对苏北盆地高邮凹陷古近系戴南组一段35件泥岩样品的稀土元素和4件碎屑岩的锆石U-Pb年代学分析,对苏北戴南组地层的物源及苏北盆地基底构造演化进行了深入探讨,恢复了沉积盆地与源区之间的耦合关系。全岩稀土元素特征表明苏北盆地古近系戴南组沉积物主要来自大别—苏鲁造山带广泛分布的新元古代浅变质酸性火成岩,具体母岩可能为高钾I型花岗片麻岩。376组协和年龄数据主要集中在2450～2600Ma、1700～2000Ma、750～850Ma、100～300Ma四个区间,其中2450～2600Ma这个年龄峰与全球新太古代晚期古陆核生长事件基本一致;1700～1900Ma这组年龄指示下扬子陆块东北部存在古元古代变质和岩浆事件,说明下扬子地块存在古元古代统一变质基底;750～850Ma这组年龄为指示扬子与华夏板块最终聚合的年龄;在100～300Ma这个年龄段中,250～300 Ma年龄锆石指示扬子地块发生裂解导致玄武岩喷发及后期伴生酸性岩浆侵入;200～250Ma为三叠纪华南陆块俯冲进入华北陆块之下形成大陆碰撞型造山带构造事件在本区的记录;100～200Ma对应于侏罗纪-白垩纪(燕山期),指示苏北盆地及周围有晚白垩纪侵入岩物源的存在,大别山-苏鲁造山带侵入岩的侵位时间可能要推迟到晚白垩世。本次测试最小年龄为94±2Ma,早于仪征运动的时间(83.5Ma),说明高邮凹陷南部陡坡带戴南组沉积物多为再旋回沉积物,沉积物来自扬子地块基底的古老岩石和大别—苏鲁造山带的新元古代浅变质岩基底,并受张八岭隆起区南段的中生代火成岩影响。
This study carried out rare earth elements analysis and U-Pb chronology dating respectively for 35mudstone samples and four clastic rock samples from the Paleogene Dainan Formation near the Gaoyou Depression in the northern Jiangsu Basin,with the aims to investigate the source of the Dainan Formation and the evolution of the basement structure of northern Jiangsu Basin and finally to restore the coupling relation between sedimentary basin and source area.Whole rock geochemical results display that the sediments in the study area was derived mainly from the Late Proterozoic low-grade metamorphic rocks in the Dabie-Sulu orogenic belt,probably the I-type high potassium granite gneiss.Cathodoluminescence(CL)images of detrital zircons reveal the most magma crystallized zircons and few overgrowth mixing zircons selected from the samples,indicating multiple-episode magma tectonic events in the study area.Zircon U-Pb ages show that there are four episodes of detrital zircons in the North Jiangsu Basin:(1)Late Paleozoic-Mesozoic(100～300Ma):igneous rocks from the Southern Zhangbaling uplift(100～200Ma),unmetamorphic rocks in the Dabie-Sulu orogenic belt(200～250 Ma),and the first phase of felsic magmatism of the Emeishan Large Igneous Province in the western margin of Yangtze platform(250～300Ma);(2)Late Proterozoic(700～850 Ma):the Late Proterozoic low-grade metamorphic granite widely distributed in the Dabie-Sulu orogenic belt;(3)Early Proterozoic(1700～1900Ma):respond to the tectonic events in the cracking of the Yangtze platform and supercontinent;(4)Late Archean-Early Proterozoic(2450～2600Ma):crystalline basement of the Yangtze platform.The minimum age of 94±2Ma obtained in this study is earlier than the time of the Yizheng Movement,suggesting that the sediments of the Dainan Formation in the southern slope of the southern Gaoyou depression mainly consists mainly of the recycled sediments,which originated mainly from the crystalline basement of the Yangtze platform and the shallow metamorphic basement of the Dabie-Sulu orogen,further affected by the Mesozoic igneous rocks in the southern part of the Zhangbaling uplift.
This study carried out rare earth elements analysis and U-Pb chronology dating respectively for 35mudstone samples and four clastic rock samples from the Paleogene Dainan Formation near the Gaoyou Depression in the northern Jiangsu Basin,with the aims to investigate the source of the Dainan Formation and the evolution of the basement structure of northern Jiangsu Basin and finally to restore the coupling relation between sedimentary basin and source area.Whole rock geochemical results display that the sediments in the study area was derived mainly from the Late Proterozoic low-grade metamorphic rocks in the Dabie-Sulu orogenic belt,probably the I-type high potassium granite gneiss.Cathodoluminescence(CL)images of detrital zircons reveal the most magma crystallized zircons and few overgrowth mixing zircons selected from the samples,indicating multiple-episode magma tectonic events in the study area.Zircon U-Pb ages show that there are four episodes of detrital zircons in the North Jiangsu Basin:(1)Late Paleozoic-Mesozoic(100～300Ma):igneous rocks from the Southern Zhangbaling uplift(100～200Ma),unmetamorphic rocks in the Dabie-Sulu orogenic belt(200～250 Ma),and the first phase of felsic magmatism of the Emeishan Large Igneous Province in the western margin of Yangtze platform(250～300Ma);(2)Late Proterozoic(700～850 Ma):the Late Proterozoic low-grade metamorphic granite widely distributed in the Dabie-Sulu orogenic belt;(3)Early Proterozoic(1700～1900Ma):respond to the tectonic events in the cracking of the Yangtze platform and supercontinent;(4)Late Archean-Early Proterozoic(2450～2600Ma):crystalline basement of the Yangtze platform.The minimum age of 94±2Ma obtained in this study is earlier than the time of the Yizheng Movement,suggesting that the sediments of the Dainan Formation in the southern slope of the southern Gaoyou depression mainly consists mainly of the recycled sediments,which originated mainly from the crystalline basement of the Yangtze platform and the shallow metamorphic basement of the Dabie-Sulu orogen,further affected by the Mesozoic igneous rocks in the southern part of the Zhangbaling uplift.
引文
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