Detrital zircon geochronology of Cambrian—Ordovician sedimentary rocks in southern Hunan—Northeast Guangxi area and its tectonic implications
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摘要: 本文利用LA-ICP-MS分析技术,对湘南-桂东北地区寒武纪和奥陶纪沉积岩进行了碎屑锆石U-Pb年代学研究。获得有效年龄数据239组,年龄值变化范围较大(3146~474 Ma),主要集中分布于2633~2473 Ma(峰值2500Ma),1880~1521 Ma(峰值1650 Ma),1146~911 Ma(峰值970 Ma),896~720 Ma(峰值800 Ma)和682~474 Ma(峰值520 Ma)5个时间段。4件样品均记录了古太古代-中太古代年龄信息,同时以1146~911 Ma和896~720 Ma两个时间段年龄最集中,反映全球Grenville造山事件和全球Rodinia超大陆裂解事件对研究区影响显著。此外,本次还获得大量泛非期(520 Ma左右)锆石年龄,认为全球泛非事件对华夏地块及其邻区影响显著,反映华夏地块与冈瓦纳大陆可能有一定亲缘性。结合前人资料,认为研究区位于华夏地块和扬子地块西南段碰撞拼合带,研究区地层同时接受两地块物质沉积,物源主要来自华夏地块。
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关键词:
- 碎屑锆石U-Th-Pb 同位素 /
- 华夏地块 /
- 扬子地块 /
- 湘南-桂东北
Abstract: In this paper, the authors studied detrital zircon geochronology of the Cambrian-Ordovician sedimentary rocks sampled from the southern Hunan to northeastern Guangxi area by using LA-ICP-MS and obtained 239 groups of effective age data, with the ages ranging from 3146 Ma to 474 Ma. Most of the data are concentrated in five periods, i.e., 2633-2473 Ma (peak value around 2500 Ma), 1880-1521 Ma (peak value around 1650 Ma), 1146-911 Ma (peak value around 970 Ma), 896-720 Ma (peak value around 800 Ma) and 682-474 Ma (peak value around 520 Ma). All the four samples recorded Paleoarchean-Mesoarchean information, and their ages are concentrated on 1146-911 Ma and 896-848 Ma, suggesting that the Grenville and Rodinia orogeny events profoundly influenced the study area. Moreover, the authors obtained a large number of ages representing the Pan-African time, implying that the global Pan-African event significantly affected the Cathaysia Block and its adjacent regions. Combined with previous researches, the authors hold that the study area is located in the southeast of the southwestern section of the collision orogenic belt between the Yangtze block and the Cathaysia block. The strata in the study area received material sources from the two blocks with the material from the Cathaysia block being dominant. -
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图 2 湘南-桂东北地区寒武纪及奥陶纪沉积岩显微照片（5倍正交镜下照相）
a—奥陶纪天马山组绢云母凝灰质细砂岩（H06）；b—奥陶纪桥亭子组伊利石-绢云母凝灰质细砂岩（H03）；c—奥陶纪黄隘组凝灰质细-粉砂岩（H08）；d—寒武纪边溪组凝灰质细砂岩（H09）；Q—石英；Ser—绢云母；Ⅰ11—伊利石
Figure 2. Microscopic photos of Cambrian and Ordovician clastic sedimentary rocks in southern Hunan-northeastern Guangxi（crossed nicols,x5）
a-Sericite fine tuffaceous sandstone from Ordovician Tianmashan Formation (H06);b-Illite-sericite tuffaceous sandstone from OrdovicianQiaotingzi Formation (H03);c-Tuffaceous fine-siltstone from Ordovician Huangai Formation (H08);d-Tuffaceous sandstone from CambrianBianxi Formation (H09)Q-Quartz;Ser-Sericite;Ⅰ11-Illite
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图 3 湘南—桂东北地区寒武纪及奥陶纪沉积岩中部分碎屑锆石CL图像
Figure 3. Feature of partially detrital zircons (CL) of Cambrian and Ordovician in south Hunan-northeast Guangxi
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图 4 湘南—桂东北地区寒武纪及奥陶纪沉积岩中碎屑锆石U−Pb年龄谐和图和年龄频率直方图
Figure 4. Zircon U−Pbconcordia diagrams and histogram diagrams of Cambrian and Ordovician in southern Hunan-northeastern Guangxi area
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图 5 A−扬子地块南部碎屑锆石统计年龄频率直方图（数据来自文献[34,79-83]）；B−华夏地块碎屑锆石统计年龄频率直方图（数据来自文献[46,56,57,75,76,84−87]）；C−湘东南地区早古生代碎屑锆石年龄频率直方图（数据来自文献[88]）；D−湘南震旦纪地层碎屑锆石年龄频率直方图（数据来自文献[34]）；E−本文研究区（湘南桂东北地区）碎屑锆石统计年龄频率直方图
Figure 5. A−Detrital zircon age frequency histogram of SouthYangtze Block (data after references [34,79-83]);B−Detritalzircon age frequency histogram of Cathaysia Block (data after references [46,56,57,75,76,84−87]);C−Detrital zircon agefrequency histogram of Early Paleozoic in south HunanProvince (data after reference [88]);D−Detrital zircon agefrequency histogram of Sinian in southern Hunan Province(data after reference [34]);E−Detrital zircon age frequency histogram of this study
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图 1 A−华南古陆残块分布图（据文献[9]改编）；B−湘南−桂东北及邻区晚寒武世−早奥陶世古地理示意图（据文献[38]改编）；C−研究区区域地质简图及采样位置图（据1:250万地质图改编）
Figure 1. A−Sketch map showing distribution of continental blocks in South China (modified after [9]);B−Palaeogeographic map ofsouthern Hunan-northeastern Guangxi and adjacent areas in the Late Cambrian to Early Ordovician (modified after [38]);C−Sketch geological map of the study area and sampling location (modified after 25 00000 geological map)
表 1 湘南—桂东北地区寒武纪及奥陶纪沉积岩中碎屑锆石U−Th−Pb同位素分析
Table 1 U−Th−Pbisotopic analyses for the detrital zircons of Cambrian and Ordovician in southern Hunan-northeasternGuangxi area
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