|
|
|
| Exploration of the technology and method of 1:50 000 regional geological survey in proluvial and alluvial plain |
| ZHAO Yong |
| Beijing Institute of Geological Survey, Beijing 100195, China |
|
|
|
|
Abstract Planning and construction work in the capital area is mainly distributed on the loose strata of the Beijing Plain,therefore, the study of Quaternary geology is particularly important. According to the 1:50 000 regional geological survey and special investigation of active faults in the Beijing Plain, the author has systematically summarized the main methods and techniques of Quaternary regional geological survey and evaluation, and the effects in solving the basic geological, ecological and environmental problems in the Quaternary. The fine geological structure of the Quaternary, distribution characteristics of aquifers, the active fault location and active time limit were accurately determined, and the evolution sequence of natural environment and human activities were discussed through regional geological survey in Beijing Plain, which also provide basis for city planning, key project construction and exploitation of water resources in emergency water sources. The results also provide important geological support for disaster reduction and prevention and research on ecological environment in evolution the capital city.
|
|
Received: 08 June 2020
|
|
|
|
|
|
[1] 北京市地质矿产局.北京市区域地质志[M].北京:地质出版社,1991:243-252.
Beijing Bureau of Geology and Mineral Resources.Annals of Regional Gelolgy of Beijing[M].Beijing:Geological Publishing House,1991:243-252.
[2] 李长安. 北京平原东北部晚新生代地层划分及地层层序初建[J].地层学杂志,1994,18(2):138-145.
Li C A.Late Cenozoic stratigraphic division and establishment of stratigraphic succession in the northeast of the Beijing plain[J].J Stratigr,1994,18(2):138-145.
[3] 袁宝印,邓成龙,吕金波,等.北京平原晚第四纪堆积期与史前大洪水[J].第四纪研究,2002,22(5):474-482.
Yuan B Y,Deng C L,Lü J B,et al.A Late Quaternary accumulation period and the prehistoric flood in Beijing plain[J].Quat Sci,2002,22(5):474-482.
[4] 赵淑君,程捷,尹功明,等.北京平原区中更新世以来的孢粉组合及其古气候意义[J].古地理学报,2008,10(6):637-646.
Zhao S J,Cheng J,Yin G M,et al.Palynological assemblages and paleoclimatic significance in Beijing plain area since the Middle Pleistocene[J].J Palaeogeogr,2008,10(6):637-646.
[5] 蔡向民,栾英波,郭高轩,等.北京平原第四系的三维结构[J].中国地质,2009,36(5):1021-1029.
Cai X M,Luan Y B,Guo G X,et al.3D Quaternary geological structure of Beijing plain[J].Geol China,2009,36(5):1021-1029.
[6] 蔡向民,郭高轩,栾英波,等.永定河形成时代研究[J].第四纪研究,2010,30(1):167-174.
Cai X M,Guo G X,Luan Y B,et al.Forming time for the Yongdinghe River[J].Quat Sci,2010,30(1):167-174.
[7] 栾英波,蔡向民,郭高轩,等.北京平原区新5孔岩心特征及地层初步划分[J].中国地质,2011,38(2):495-503.
Luan Y B,Cai X M,Guo G X,et al.Core characteristics and preliminary stratigraphic classification of the New-5 hole in Beijing plain[J].Geol China,2011,38(2):495-503.
[8] 蔡向民,郭高轩,张磊,等.北京城湖泊的成因[J].中国地质,2013,40(4):1092-1098.
Cai X M,Guo G X,Zhang L,et al.The origin of lakes in Beijing city[J].Geol China,2013,40(4):1092-1098.
[9] 赵勇,蔡向民,王继明,等.北京平原顺义ZK12-2钻孔剖面第四纪磁性地层学研究[J].地质学报,2013,87(2):288-294.
Zhao Y,Cai X M,Wang J M,et al.Quaternary magnetostratigraphy of the Shunyi area in Beijing plain using ZK12-2 borehole profile[J].Acta Geol Sin,2013,87(2):288-294.
[10] 蔡向民,张磊,郭高轩,等.北京平原地区第四纪地质研究新进展[J].中国地质,2016,43(3):1055-1066.
Cai X M,Zhang L,Guo G X,et al.New progress in the study of Quaternary geology in Beijing plain[J].Geol China,2016,43(3):1055-1066.
[11] 张磊,何静,白凌燕,等.北京凹陷北缘第四纪凹陷盆地沉积速率变化特征与顺义断裂活动性的响应关系[J].中国地质,2016,43(2):511-519.
Zhang L,He J,Bai L Y,et al.The response relationship between the variation characteristics of deposition rate of Quaternary depression basin on the northern margin of Beijing depression and the activity of Shunyi fault[J].Geol China,2016,43(2):511-519.
[12] 周毅,郭高轩,张磊,等.北京后沙峪凹陷的第四纪地层划分与构造演化[J].中国地质,2016,43(3):1067-1075.
Zhou Y,Guo G X,Zhang L,et al.The division of Quaternary strata and tectonic evolution in Houshayu Sag of Beijing[J].Geol China,2016,43(3):1067-1075.
[13] 赵勇,王强,李瑞杰,等.北京平原区南部PGZ01孔第四纪地层划分及其环境意义[J].古地理学报,2018,20(2):337-348.
Zhao Y,Wang Q,Li R J,et al.Quaternary stratigraphic division and its environmental significance of borehole PGZ01 in southern Beijing plain area[J].J Palaeogeogr,2018,20(2):337-348.
[14] 王强,张玉发,袁桂邦,等.MIS 3阶段以来河北黄骅北部地区海侵与气候期对比[J].第四纪研究,2008,28(1):79-95.
Wang Q,Zhang Y F,Yuan G B,et al.Since MIS 3 stage the correlation between transgression and climatic changes in the north Huanghua area,Hebei[J].Quat Sci,2008,28(1):79-95.
[15] 王强. 渤海西岸全新世早期基底泥炭堆积时间域初步研究[J].第四纪研究,1999,19(1):91.
Wang Q.Preliminary study on the time domain of basal peat accumulation in the early Holocene in the West Bohai Bay[J].Quat Sci,1999,19(1):91.
[16] Toker E,Kayseri-Özer M S,Özkul M,et al.Depositional system and palaeoclimatic interpretations of Middle to Late Pleistocene travertines:Kocaba?,Denizli,South-West Turkey[J].Sedimentology,2015,62(5):1360-1383.
[17] 高秀林,王强,李玉德,等.从天津P8孔看中更新世末期以来海侵期、气候期对比问题[J].海洋地质与第四纪地质,1986,6(1):53-64,131.
Gao X L,Wang Q,Li Y D,et al.On correlations between transgressions and climatic phases since late Middle-Pleistocene based on data of drilling hole P8 in Tinjin[J].Mar Geol Quat Geol,1986,6(1):53-64,131.
[18] Yao Z Q,Shi X F,Liu Q S,et al.Paleomagnetic and astronomical dating of sediment core BH08 from the Bohai Sea,China:Implications for glacial-interglacial sedimentation[J].Palaeogeogr Palaeoclimatol Palaeoecol,2014,393:90-101.
[19] 袁璐璐,汪明启,胡佳乐.第四纪沉积物测年新进展[J].中国地质调查,2014,1(1):46-51.
Yuan L L,Wang M Q,Hu J L.New progress in dating of Quaternary sediments[J].Geol Surv China,2014,1(1):46-51.
[20] 蒋仁,于俊杰,劳金秀,等.长江三角洲北翼ZKA4钻孔剖面第四纪磁性地层特征及其意义[J].中国地质调查,2015,2(7):30-34.
Jiang R,Yu J J,Lao J X,et al.Characteristics and implications of the Quaternary magnetostratigraphy in borehole ZKA4 from the northern flank of Yangtze River delta[J].Geol Surv China,2015,2(7):30-34.
[21] 白凌燕,张磊,蔡向民,等.磁性地层年代对北京平原顺义断裂第四纪活动性的约束[J].现代地质,2014,28(6):1234-1242.
Bai L Y,Zhang L,Cai X M,et al.Quaternary magnetostratigraphic time framework constraints on activity characteristics of the Shunyi fault,Beijing plain[J].Geoscience,2014,28(6):1234-1242.
[22] Singer B S.A Quaternary geomagnetic instability time scale[J].Quat Geochronol,2014,24:29-52.
[23] 张磊,白凌燕,蔡向民,等.北京平原南口—孙河断裂带北西段活动性分析[J].中国地质,2014,41(3):902-911.
Zhang L,Bai L Y,Cai X M,et al.An analysis of the activity of the northwest part of Nankou-Sunhe fault[J].Geol China,2014,41(3):902-911. |
| [1] |
ZHANG Jiajia, ZHANG Shunlin, WANG Qingsong, GU Danian. Application of comprehensive geophysical prospecting method in ore prospecting in coverage area: A case study of integrated survey area of Wuhe Gold Mine in Eastern Anhui[J]. , 2020, 7(6): 109-115. |
| [2] |
TIE Yongbo, XU Ruge, LIU Hong, WANG Jiazhu, BA Renji, XIANG Anping, YANG Jian, OUYANG Yuan, ZHANG Yu, WANG Hong. Study on the characteristics and formation mechanism of the typical post-fire debris flow in Lushan area of Xichang City: A case study of 3# branch on the left bank of Xiangshuigou[J]. , 2020, 7(3): 82-88. |
| [3] |
WANG Weiping, WU Chengping, MA Xunbiao. Aeromagnetic field feature and iron ore target prospecting in deep coverage area of Qihe in Shandong Province[J]. , 2020, 7(1): 23-29. |
| [4] |
WANG Qingsong, ZHANG Jiajia, ZHANG Shunlin, ZHU Yikun, ZHANG Jinhui, HAO Shuxi. Important discoveries in Wuhe integrated exploration gold mine area in Anhui Province and its geological significance[J]. , 2019, 6(2): 26-33. |
| [5] |
WNAG Denghong, SUN Yan, LIU Xifang, TIAN Shihong, DAI Jingjing, LIU Lijun, MA Shengchao. Deep exploration technology and prospecting direction for lithium energy metal[J]. , 2018, 5(1): 1-9. |
| [6] |
WANG Jingui, ZHANG Xinquan, LI Dian, ZHANG Xinzheng, BAI Chundong, ZHANG Zixuan, TIAN Lifu. Application of comprehensive method to search concealed deposit in the shallow area of Hanggaiyinhundi area in Inner Mongolia[J]. , 2016, 3(4): 69-75. |
|
|
|
|
2021, Vol. 8 
