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物探与化探  2023, Vol. 47 Issue (1): 55-64    DOI: 10.11720/wtyht.2023.1005
  地质调查·资源勘查 本期目录 | 过刊浏览 | 高级检索 |
鲁北平原南部QK4钻孔岩心特征及第四纪地层划分
周永刚1,2(), 戴黎明3,4, 田振环1,2, 于春楠1,2, 张振飞1,2,5, 刘伟1,2, 裴伦培1,2
1.山东省第一地质矿产勘查院,山东 济南 250109
2.山东省富铁矿勘查技术开发工程实验室,山东 济南 250109
3.中国海洋大学 海洋地球科学学院,山东 青岛 266100
4.青岛海洋科学与技术试点国家实验室 海洋矿产资源评价与探测技术功能实验室,山东 青岛 266237
5.昆明理工大学 国土资源工程学院,云南 昆明 650093
Core characteristics and Quaternary stratigraphic division of borehole QK4 in southern Lubei Plain
ZHOU Yong-Gang1,2(), DAI Li-Ming3,4, TIAN Zhen-Huan1,2, YU Chun-Nan1,2, ZHANG Zhen-Fei1,2,5, LIU Wei1,2, PEI Lun-Pei1,2
1. No.1 Institute of Geology and Mineral Resources of Shandong Province, Jinan 250109, China
2. Shandong Engineering Laboratory for High-Grade Iron Ore Exploration and Exploitation, Jinan 250109, China
3. College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
4. Functional Laboratory of Marine Mineral Resources Evaluation and Exploration Technology, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China
5. Kunming University of Science and Technology, Kunming 650093, China
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摘要 

第四纪地层格架的建立对区域地层对比及古地理环境演化研究具有重要意义,区域上晚更新世以来的地层已被广泛研究,但对完整的第四纪地层格架研究不足。为此,对鲁北平原QK4钻孔(深度285.98 m)进行了古地磁、AMS 14C、OSL、测井、岩石地层等研究。在系统的古地磁采集(398件)、处理和测试的基础上,认为岩心记录了布容正极性时(Brunhes)、松山负极性时(Matuyama)、高斯正极性时(Gauss)及其中的部分极性亚时。在磁性年代框架的基础上,结合AMS 14C、OSL、测井及岩石地层特征,对钻孔揭露的第四纪地层进行了划分,确定了全新统、上更新统、中更新统、下更新统的底界分别位于4.11、23.49、118.70、147.35 m,钻孔揭露的地层从上向下依次为新生界黑土湖组、大站组、平原组和明化镇组。研究结果建立了鲁北平原南部第四纪地层格架,为该区第四纪地层划分对比、古地理环境演化等提供了可靠的岩石学、年代学、古地磁学证据。

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周永刚
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张振飞
刘伟
裴伦培
关键词 鲁北平原古地磁AMS 14C测年OSL测年第四纪    
Abstract

The establishment of the Quaternary stratigraphic framework is of great significance for the study of regional stratigraphic correlation and paleogeographic environment evolution. The sedimentary strata since the Late Pleistocene have been extensively studied, but the research on the complete Quaternary stratigraphic framework is not yet sufficient. Therefore, paleomagnetic, AMS 14C, OSL, well logging, and lithostratigraphic studies were conducted on borehole QK4 (depth: 285.98 m) in the Lubei Plain. Based on the systematic paleomagnetic sampling (398 samples), processing, and testing, it is considered that the cores from borehole QK4 recorded Brunhes normal polarity chron, Maruyama reversed polarity chron, Gauss normal polarity chron, and some of their polarity subchrons. Based on the magnetic age framework, as well as MS 14C, OSL, well logging, and lithostratigraphic characteristics, the Quaternary strata revealed by borehole QK4 were divided, and it was determined that the bottom boundaries of the Holocene, Upper Pleistocene, Middle Pleistocene, and Lower Pleistocene strata have depths of 4.11 m, 23.49 m, 118.70 m, and 147.35 m, respectively. Moreover, as the strata revealed, the strata revealed by borehole QK4 include the Cenozoic Heituhu, Dazhan, Pingyuan, and Minghuazhen formations from top to bottom. The results allowed for the establishment of the Quaternary stratigraphic framework in the southern Lubei Plain, thus providing reliable petrological, chronological, and paleomagnetic evidence for the Quaternary stratigraphic division and correlation and palaeogeographic environmental evolution in the southern Lubei Plain.

Key wordsLubei Plain    palaeomagnetism    AMS 14C dating    OSL dating    Quaternary
收稿日期: 2022-01-22      修回日期: 2022-02-23      出版日期: 2023-02-20
ZTFLH:  P631  
基金资助:山东省地质勘查基金项目“山东省1:5万长山、桓台县、淄博市幅区域地质调查”(鲁勘字(2013)64号)
作者简介: 周永刚(1983-),男,硕士,高级工程师,主要从事区域地质调查与矿产勘查、遥感地质等工作。Email:187346471@qq.com
引用本文:   
周永刚, 戴黎明, 田振环, 于春楠, 张振飞, 刘伟, 裴伦培. 鲁北平原南部QK4钻孔岩心特征及第四纪地层划分[J]. 物探与化探, 2023, 47(1): 55-64.
ZHOU Yong-Gang, DAI Li-Ming, TIAN Zhen-Huan, YU Chun-Nan, ZHANG Zhen-Fei, LIU Wei, PEI Lun-Pei. Core characteristics and Quaternary stratigraphic division of borehole QK4 in southern Lubei Plain. Geophysical and Geochemical Exploration, 2023, 47(1): 55-64.
链接本文:  
https://www.wutanyuhuatan.com/CN/10.11720/wtyht.2023.1005      或      https://www.wutanyuhuatan.com/CN/Y2023/V47/I1/55
Fig.1  鲁北平原构造简图(底图据[14??-17]修改)
序号 样品号 埋深/m 岩性 分析结果 备注
现代碳百分数/% 表观年龄/ka
1 QK4-Z1 0.7~1.0 极深灰色含有机质粘土 44.11±2.45 6.77±0.46
Table 1  QK4钻孔AMS 14C测年结果
序号 样品号 埋深/m U/ppm Th/ppm K/% 等效剂量
E.D(Gy)
含水量
/%
年龄/ka 备注
1 QK4-GS1 1.5~1.8 2.83±0.10 12.0±0.31 1.73±0.06 18.34±0.79 15.1 4.8±0.3
2 QK4-GS2 14.05~14.25 2.06±0.08 9.41±0.27 1.75±0.06 239.80±3.50 16.8 75.2±3.4
3 QK4-GS11 203~203.2 2.08±0.09 10.2±0.29 1.86±0.06 560.02±12.41 16.6 >169.0 生长曲线
趋于饱和
Table 2  QK4钻孔光释光测年结果
Fig.2  QK4孔岩性柱、自然伽马、电阻率、密度、自然电位及沉积环境分析
序号 深度/m 实测极性层 标准极性带 极性亚时 年代/Ma
1 0~23.49 N1 Brunhes
2 23.49~26.44 R1 Blake 0.12
3 26.44~28.40 N2
4 28.40~29.58 R2 Cr0 0.260
5 29.58~32.10 N3
6 32.10~33.75 R3 Cr1 0.319
7 33.75~65.18 N4
8 65.18~66.88 R4 Cr2 0.543
9 66.88~72.96 N5
10 72.96~75.08 R5 Cr3 0.593
11 75.08~116.59 N6 0.781
12 116.59~120.43 R6 Matuyama
13 120.43~123.42 N7
14 123.42~129.31 R7
15 129.31~134.17 N8 Olduvai 1.77~1.95
16 134.17~141.54 R8
17 141.54~144.69 N9
18 144.69~147.39 R9 2.588
19 147.39~171.25 N10 Gauss
20 171.25~173.77 R10 Kaena 3.032~3.116
21 171.25~217.54 N11
22 217.54~221.57 R11 Mammoth 3.207~3.330
23 221.57~285.98 N12
Table 3  QK4钻孔古磁性分析结果对比
Fig.3  QK4钻孔磁性地层
Fig.4  钻孔岩心及野外剖面特征
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