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| 3D spatial distribution of Quaternary sedimentary strata in Zhengzhou |
| WANG Yongcheng1, ZHANG Bingchen2,4, LI Qingkang2,4, REN Liping2,4, XU Lianfeng1, SONG Lei3, FAN Xiaolei2 |
1. Henan Institute of Geological Sciences Co., Ltd., Henan Zhengzhou 450001, China;
2. Henan Institute of Geology, Henan Zhengzhou 450001, China;
3. Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Hebei Shijiazhaung 050000, China;
4. Henan Geological Research Institute Geoscience Popularization Base, Henan Zhengzhou 450001, China |
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Abstract The study of the spatial distribution characteristics and law of Quaternary sedimentary strata in Zhengzhou is closely related to the birth and development of early human civilization along Yellow River, especially in the surrounding areas of Zhengzhou. And, it also plays an important supporting role in modern urban planning and layout, underground space development and utilization, as well as the ecological protection and high-quality development of Yellow River. Thus, the geological tourism and geological cultural resources survey was carried out in Zhengzhou, and 38 sedimentary boreholes were drilled in the main urban area of Zhengzhou and different geomorphic units around it, including 9 deep boreholes exposing Quaternary period. Based on the results of deep drilling and existing HKGA borehole exploration results, the authors established the standard stratigraphic columns of various geomorphic units, through accurately dividing the Quaternary sedimentary stratigraphic structure of each borehole. By analyzing and comparing the changing characteristics of sedimentary strata in these different geomorphic units, the authors obtained the understanding and empirical evidence, that is aeolian sedimentation was commonly present in Early and Middle Pleistocene in the eastern plain area, and it transformed into river and lacustrine facies sedimentation in Late Pleistocene. Based on the analysis of sediment source characteristics, it has indirectly confirmed that the sedimentation time of Yellow River sediment in this area may have started from the Late Pleistocene period.
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Received: 22 April 2023
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[1] 杨伦,刘少锋,王家生.普通地质学简明教程[M].北京:中国地质大学出版社,1998:182-188.
Yang L,Liu S F,Wang J S.A Concise Course in General Geo-logy[M].Beijing:China University of Geosciences Press,1998:182-188.
[2] 孙枢,王成善.“深时”(Deep Time)研究与沉积学[J].沉积学报,2009,27(5):792-810.
Sun S,Wang C S.Deep time and sedimentology[J].Acta Sedimentologica Sinica,2009,27(5):792-810.
[3] 苏晶文,龚建师,李运怀,等.基于地层结构组合的第四纪地质单元划分研究——以皖江经济带沿江丘陵平原区为例[J].中国地质调查,2019,6(5):28-35.
Su J W,Gong J S,Li Y H,et al.Division of Quaternary geological units based on stratigraphic architecture combination:A case study in Wanjiang River Economic Zone[J].Geological Survey of China,2019,6(5):28-35.
[4] 陈宏强,杨瑞,李庆喆,等.河北唐山西部PZK14孔晚新生代沉积演化特征[J].中国地质调查,2022,9(3):67-75.
Chen H Q,Yang R,Li Q Z,et al.Sedimentary evolution of borehole PZK14 in western Tangshan area during Late Cenozoic[J].Geological Survey of China,2022,9(3):67-75.
[5] 徐海亮,王朝栋.史前郑州地区黄河河流地貌与新构造活动关系初探[J].华北水利水电学院学报,2010,31(6):101-106.
Xu H L,Wang C D.Preliminary study on the relationship between the fluvial geomorphology and the neotectonic movement in Yellow River in Zhengzhou prehistoric times[J].Journal of North China Institute of Water Conservancy and Hydroelectric Power,2010,31(6):101-106.
[6] 董晓光,田洪礼.从环境地质角度议郑州市城建发展布局[J].河南地质,2000,18(2):152-157.
Dong X G,Tian H L.A study related to development distribution of Zhengzhou urban construction from environmental geology[J].Henan Geology,2000,18(2):152-157.
[7] 朱晓强,王强恒.郑州市地质环境适宜性评价及功能区划[J].安全与环境工程,2013,20(2):86-90.
Zhu X Q,Wang Q H.Suitability evaluation and function zoning of geological environment in Zhengzhou City[J].Safety and Environmental Engineering,2013,20(2):86-90.
[8] 张军龙,申晋利,田勤俭,等.邙山东侧地貌陡坎与老鸦陈断层活动性关系讨论[J].地震,2008,28(4):121-127.
Zhang J L,Shen J L,Tian Q J,et al.Relationship between Mangshan geomorphic scarp and Laoyachen fault activity[J].Earthquake,2008,28(4):121-127.
[9] 章秉辰,李庆康.邙山黄土特征及区域对比研究[M].北京:地质出版社,2018:53-109.
Zhang B C,Li Q K.Study on Characteristics and Regional Comparison of Mangshan Loess[M].Beijing:Geology Press,2018:53-109.
[10] 章秉辰. 从风中走来的高原[J].自然资源科普与文化,2021(2):34-41.
Zhang B C.A plateau coming from the wind[J].Scientific and Cultural Popularization of Natural Resources,2021(2):34-41.
[11] 张宗祜,张之一,王芸生.中国黄土[M].北京:地质出版社,1989:87-98.
Zhang Z H,Zhang Z Y,Wang Y S.Loess in China[M].Beijing:Geology Press,1989:87-98. |
| [1] |
CHEN Hongqiang, YANG Rui, LI Qingzhe, ZHAO Huaping, DUAN Bingxin, LIU Beibei, ZHUAN Shaopeng, CHEN Chao. Sedimentary evolution of borehole PZK14 in western Tangshan area during Late Cenozoic[J]. , 2022, 9(3): 67-75. |
| [2] |
LUO Wei. Evaluation of groundwater resources quantity in Lingyun County of Guangxi[J]. , 2022, 9(1): 91-103. |
| [3] |
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| [4] |
ZHAO Jichu, GUO Guoqiang, WU Qinghua. Application of comprehensive geophysical prospecting method in uplift geothermal field[J]. , 2021, 8(3): 21-29. |
| [5] |
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| [6] |
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Borehole ZKA4 from the Northern Flank of Yangtze River Delta[J]. , 2015, 2(7): 30-34. |
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2023, Vol. 10 
