首页 | 本学科首页   官方微博 | 高级检索  
     

松辽盆地北部上二叠统林西组古生物年代学、地球化学特征及地质意义
引用本文:张海华,李晓海,张健,郑月娟,陈树旺,张德军,苏飞,卞雄飞,孙雷. 松辽盆地北部上二叠统林西组古生物年代学、地球化学特征及地质意义[J]. 现代地质, 2021, 35(2): 568-578. DOI: 10.19657/j.geoscience.1000-8527.2021.040
作者姓名:张海华  李晓海  张健  郑月娟  陈树旺  张德军  苏飞  卞雄飞  孙雷
作者单位:中国地质调查局沈阳地质调查中心,辽宁 沈阳 110034
基金项目:中国地质调查局项目(DD20160163);中国地质调查局项目(DD20190097)
摘    要:对松辽盆地北部地区黑富地l井钻遇的上二叠统林西组碎屑岩样品进行微体化石以及主量元素、微量元素和稀土元素测试分析,进而探讨该区林西组时代、地球化学特征、沉积环境及构造背景.获得的Protohaploxypinus fertilis-Piceaepollenites opimus-Alisporites communis孢...

关 键 词:松辽盆地  林西组  孢粉  地球化学  构造背景
收稿时间:2020-11-30
修稿时间:2021-02-20

Paleochronology,Geochemical Characteristics,and Geological Significance of the Upper Permian Linxi Formation in the Northern Songliao Basin
ZHANG Haihua,LI Xiaohai,ZHANG Jian,ZHENG Yuejuan,CHEN Shuwang,ZHANG Dejun,SU Fei,BIAN Xiongfei,SUN Lei. Paleochronology,Geochemical Characteristics,and Geological Significance of the Upper Permian Linxi Formation in the Northern Songliao Basin[J]. Geoscience of Geosciences, 2021, 35(2): 568-578. DOI: 10.19657/j.geoscience.1000-8527.2021.040
Authors:ZHANG Haihua  LI Xiaohai  ZHANG Jian  ZHENG Yuejuan  CHEN Shuwang  ZHANG Dejun  SU Fei  BIAN Xiongfei  SUN Lei
Affiliation:Shenyang Center of Geological Survey, China Geological Survey, Shenyang, Liaoning 110034, China
Abstract:The paleontological fossils, major and trace elements (including rare earth elements (REEs)) of the Upper Permian Linxi Formation (Fm.) clastic rocks in well Heifudi 1 in the northern Songliao Basin were analyzed, in order to explore the age, geochemical characteristics, sedimentary environment, and tectonic background of the Linxi Formation. The Protohaploxypinus fertilis, Piceaepollenites opimus, and Alisporites communis palynological fossil assemblages obtained in this study indicate that the stratigraphic age is Late Permian. The average content of major elements is SiO2=60.41%, CaO=3.65%, Al2O3=16.36%, K2O=2.69%, Na2O=3.25%, K2O/Na2O=0.40-7.01, and A12O3/(CaO+Na2O)=0.92-6.89. The total REE (ΣREE) contents are of 63.20×10-6-208.05×10-6(average 147.56×10-6), with mainly negative Eu anomalies (δEu) of 0.56-1.34 (average 0.73) and weakly-negative Ce anomalies (δCe=0.90-0.98). The clastic rocks are characterized by LREE enrichments and HREE depletions. The trace element contents are characterized by depletions in Nb, Ta, and Sr, and enrichments in Rb, Ba, La, Sm, Pb, and Nd. Geochemical features of the clastic rocks and the discrimination diagrams of La/Th-Hf and TiO2- Ni show that the Linxi Formation has diverse sediment sources, mainly from upper-crustal felsic rocks and minor from mafic rocks. The primitive-mantle normalized multi-element and chondrite-normalized REE diagrams, K2O/Na2O-SiO2 plot, together with tectonic discrimination functions (F1, F2) and geochemical parameters indicate that the northern Songliao basin provenance source region was largely in an active continental margin and continental island arc setting, whilst the sedimentary facies was transitioned from marine-terrestrial to terrestrial.
Keywords:Songliao Basin  Linxi Formation  spores and pollen  geochemistry  tectonic setting  
点击此处可从《现代地质》浏览原始摘要信息
点击此处可从《现代地质》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号