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北京大兴凸起南部PGZ05钻孔剖面第四纪磁性地层学
引用本文:赵勇,李瑞杰,魏波,王纯君,孙永华,方同明.北京大兴凸起南部PGZ05钻孔剖面第四纪磁性地层学[J].现代地质,2019,33(1):56-62.
作者姓名:赵勇  李瑞杰  魏波  王纯君  孙永华  方同明
作者单位:北京市地质调查研究院,北京 100195
基金项目:中国地质调查局项目“北京1∶5万琉璃河、庞各庄、安次县幅区域地质调查”(12120114007701)
摘    要:对北京大兴凸起南部PGZ05孔(孔深255 m)全孔岩心进行了磁性地层、岩石地层、AMS14C测年研究,在系统性的古地磁样品采集(440块岩样)、处理和测试基础上,分析认为255 m的岩心记录了布容正向极性时(Brunhes)、贾拉米洛(Jaramillo)极性亚时、奥尔都维(Olduvai)极性亚时和高斯正极性时(Gauss)。在此磁性年代框架上,结合AMS14C测年及岩性特征,对PGZ05钻孔剖面进行第四纪地层划分,确定下更新统、中更新统、上更新统和全新统的分布深度及年代,将更新统的底界(Q/N)定位于181. 35 m处,亦为一重要岩性(棕红色半固结黏土)界限,中更新统、上更新统、全新统的底界分别定位于75. 60 m、57. 20 m、17. 35 m处。研究成果为大兴凸起南部第四纪地层划分与对比、古地理环境演变及区域地层研究提供了可靠的地层年代学框架,具有重要地质意义。

关 键 词:磁性地层  第四纪  大兴凸起南部  AMS14C测年
收稿时间:2018-01-23
修稿时间:2018-09-05

Magnetostratigraphy of Borehole PGZ05 in Southern Daxing Uplift,Beijing Plain
ZHAO Yong,LI Ruijie,WEI Bo,WANG Chunjun,SUN Yonghua,FANG Tongming.Magnetostratigraphy of Borehole PGZ05 in Southern Daxing Uplift,Beijing Plain[J].Geoscience——Journal of Graduate School,China University of Geosciences,2019,33(1):56-62.
Authors:ZHAO Yong  LI Ruijie  WEI Bo  WANG Chunjun  SUN Yonghua  FANG Tongming
Institution:Beijing Geological Survey Institute,Beijing 100195,China
Abstract:Quaternary deposits in the southern Daxing uplift in the Beijing Plain provide an important archive for Quaternary stratigraphic changes. Here we present the magnetostratigraphic results of borehole PGZ05 (255 m). A total of 440 undisturbed samples were collected from the borehole at a 0.2-0.5 m interval except for the sand and gravel lay. The results show that the Brunhes/Matuyama and Matuyama/Gauss boundaries occur at 75.60 m and 181.35 m deep, respectively. The Gauss normal polarity chron occurs at 181.35 to 255.00 m deep. The 75.60 to 181.35 m interval is fairly correlative with the Matuyama reversal in the geomagnetic polarity timescale, with two normal polarity zones corresponding to the Jaramillo (90.90-100.60 m) and Olduvai (149.70~165.50 m) subchrons, respectively. The AMS14C age of (2,370±30) a BP and (23,190±100) a BP were obtained from the samples at 12.20 m and 31.45 m deep. The lithologic section of the borehole PGZ05 includes the entire Pleistocene and Holocene sequences and part of the Pliocene sequence. According to the M/G boundary and lithologic section of the borehole, we suggest that the N/Q boundary is located at 181.35 m deep, and it represents an important lithological interface. We propose that the sediments below 181.35 m depth belong to the Upper Pliocene series. The Lower Pleistocene sequence occurs at 75.60-181.35 m deep and were deposited during 0.78-2.58 Ma. The boundary between the Middle and Upper Pleistocene sequence is located at 57.20 m deep, whilst the Holocene-Upper Pleistocene boundary is located at 17.35 m deep.
Keywords:magnetostratigraphy  Quaternary  southern Daxing uplift  AMS14C dating  
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