渤海湾西MIS3阶段海侵边界探讨

doi:10.19388/j.zgdzdc.2021.01.10

Abstract
Figure/Table
References
Related Citation (12)

Download: PDF (4635 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS)

Abstract The Southern Tianjin Plain, located in the western coast of Bohai Bay, is an ideal natural place to study the transgression and sea level change. Based on the comprehensive research of sedimentary characteristics, dating (AMS ¹⁴C) and micro paleontology of two boreholes (ZKQ1 and ZK1), the authors inferred that transgression maximum influence boundary in the MIS 3 stage was between two boreholes (ZK1 and ZKQ1). The western side of the boundary is continental sedimentary, and the eastern side of the boundary is transitional sedimentary. boundry location was in the area of the present Heilonggang River and was once an ancient river channel, so it is speculated that the area affected by the transgression in this period was restricted by the ancient river channel. Combined with the previous three boreholes (ZKQ4, CGZ5 and CGZ7) data, the author has established the profile of the E→W direction (sea → land) and further confirmed that E→W in this area was transformed from Marine facies (CGZ7 and CGZ5) to transitional sedimentary (ZKQ4 and ZKQ1) to continental facies (ZK1). It is speculated that the transgression boundary of MIS3 is in the area of Dongshangmatou (CGZ5) and Gaojiazhuang (ZKQ4) in Jinghai district. This achievement is of great significance to the restoration of paleogeographic evolution, the sea-level change research and the geological exploration of hydraulic environment in this region.

Key words： Bohai Bay transgression dating MIS3 stage sedimentary environment

Received: 22 May 2020

P534.63

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	LU Qingwei

Cite this article:

LU Qingwei. Discussion on the transgression boundary of MIS3 stage in the western coast of Bohai Bay[J]. , 2021, 8(1): 89-96.

URL:

http://journal25.magtechjournal.com/Jwk_dzdc/EN/10.19388/j.zgdzdc.2021.01.10 OR http://journal25.magtechjournal.com/Jwk_dzdc/EN/Y2021/V8/I1/89

[1] 自然资源部.2019年中国海平面公报[R].北京:自然资源部,2020.
Ministry of Natural Resources.Sea level bulletin of China in 2019[R].Beijing:Ministry of Natural Resources of the People’s Republic of China,2020.
[2] 联合国政府间气候变化专门委员会.气候变化中的海洋和冰冻圈特别报告[R].2019.
IPCC.Special report on the ocean and cryosphere in a changing climate[R].2019.
[3] 蔡榕硕,谭红建.海平面加速上升对低海拔岛屿、沿海地区及社会的影响和风险[J].气候变化研究进展,2020,16(2):163-171.
Cai R S,Tan H J.Impacts and risks of accelerating sea level rise on low lying islands,coasts and communities[J].Climate Change Res,2020,16(2):163-171.
[4] 杜晓敏,周平,常勇,等.美国海岸带综合地质调查进展及其对中国海岸带研究的启示[J].地质通报,2020,39(2/3):414-423.
Du X M,Zhou P,Chang Y,et al.A review on Coastal and Marine Geology Program of U.S.Geological Survey and some suggestions on coastal studies in China[J].Geol Bull China,2020,39(2/3):414-423.
[5] 赵松龄,杨光复,苍树溪,等.关于渤海湾西岸海相地层与海岸线问题[J].海洋与湖沼,1978,9(1):15-25.
Zhao S L,Yang G F,Cang S X,et al.On the marine stratigraphy and coastlines of the western coast of the gulf of Bohai[J].Oceanol Limnol Sin,1978,9(1):15-25.
[6] 汪品先,闵秋宝,卞云华,等.我国东部第四纪海侵地层的初步研究[J].地质学报,1981,55(1):1-13.
Wang P X,Min Q B,Bian Y H,et al.Strata of quaternary transgressions in east China:a preliminary study[J].Acta Geol Sin,1981,55(1):1-13.
[7] 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.
[8] 王强,李从先.中国东部沿海平原第四系层序类型[J].海洋地质与第四纪地质,2009,29(4):39-51.
Wang Q,Li C X.The type of Quaternary sequence in the east China coastal plain[J].Mar Geol Quat Geol,2009,29(4):39-51.
[9] 施林峰,翟子梅,王强,等.从天津CQJ4孔探讨中国东部海侵层的年代问题[J].地质论评,2009,55(3):375-383.
Shi L F,Zhai Z M,Wang Q,et al.Geochronological study on transgression layers of the CQJ4 borehole at Dagang area in Tianjin,China[J].Geol Rev,2009,55(3):375-383.
[10] 胥勤勉,袁桂邦,张金起,等.渤海湾沿岸晚第四纪地层划分及地质意义[J].地质学报,2011,85(8):1352-1367.
Xu Q M,Yuan G B,Zhang J Q,et al.Stratigraphic division of the Late Quaternary strata along the coast of Bohai Bay and its geology significance[J].Acta Geol Sin,2011,85(8):1352-1367.
[11] 陈永胜,王宏,裴艳东,等.渤海湾西岸晚第四纪海相地层划分及地质意义[J].吉林大学学报:地球科学版,2012,42(3):747-759.
Chen Y S,Wang H,Pei Y D,et al.Division and its geological significance of the Late Quaternary marine sedimentary beds in the west coast of Bohai Bay,China[J].J Jilin Univ (Earth Sci Ed),2012,42(3):747-759.
[12] 高峰,胥勤勉,袁桂邦,等.渤海湾北岸TZ02孔晚新生代沉积环境演化过程[J].第四纪研究,2017,37(3):667-678.
Gao F,Xu Q M,Yuan G B,et al.Sedimentary environment evolution of borehole TZ02 in the northern Bohai Bay during Late Cenozoic[J].Quat Sci,2017,37(3):667-678.
[13] 鲁庆伟,王强,詹健,等.渤海湾西岸沧县隆起中更新世地层间断[J].古地理学报,2018,20(4):665-679.
Lu Q W,Wang Q,Zhan J,et al.Middle Pleistocene stratigraphic hiatus on the Cangxian Uplift,the west coast of Bohai Bay[J].J Palaeogeogr,2018,20(4):665-679.
[14] 鲁庆伟,王西玉,贾超,等.渤海湾西沧县隆起第四纪以来沉积差异性研究[J].地质找矿论丛,2020,35(1):95-101.
Lu Q W,Wang X Y,Jia C,et al.Study on sedimentary difference at the Cangxian uplift in the west coast of Bohai Bay since the Quaternary period[J].Contrib Geol Miner Resour Res,2020,35(1):95-101.
[15] 王强,袁桂邦,张熟,等.渤海湾西岸贝壳堤堆积与海陆相互作用[J].第四纪研究,2007,27(5):775-786.
Wang Q,Yuan G B,Zhang S,et al.Shelly ridge accumulation and sea-land interaction on the west coast of the Bohai bay[J].Quat Sci,2007,27(5):775-786.
[16] 王宏,陈永胜,田立柱,等.渤海湾全新世贝壳堤与牡蛎礁:古气候与海面变化[J].地质通报,2011,30(9):1405-1411.
Wang H,Chen Y S,Tian L Z,et al.Holocene cheniers and oyster reefs in Bohai Bay:palaeoclimate and sea level changes[J].Geol Bull China,2011,30(9):1405-1411.
[17] 岳军,Dong Y张宝华,等.渤海湾西岸的几道贝壳堤[J].地质学报,2012,86(3):522-534.
Yue J,Dong Y,Zhang B H,et al.A few of barrier sand-bars on the west coast of Bohai Bay[J].Acta Geol Sin,2012,86(3):522-534.
[18] 李凤林. 渤海湾西岸环境地质图集[CM].北京:地质出版社,2016:35-38.
Li F L.Atlas of environment geology on the west coast of Bohai Bay[CM].Beijing:Geological Publishing House,2016:35-38.
[19] 方晶,胡克,张国艳,等.渤海湾西岸全新世最大海侵位置探讨——以天津市西南精武镇一带为例[J].海岸工程,2012,31(3):45-54.
Fang J,Hu K,Zhang G Y,et al.Discussion of maximum Holocene transgression location on the west coast of the Bohai Bay:Taking the Jingwu town southwest of Tianjin as an example[J].Coast Eng,2012,31(3):45-54.
[20] 刘艳霞,黄海军,董慧君,等.渤海西南岸全新世最大海侵界线及其地貌特征[J].第四纪研究,2015,35(2):340-353.
Liu Y X,Huang H J,Dong H J,et al.Geomorphic characteristics and location of the maximum Holocene transgression boundary in the southwestern coast of the Bohai sea[J].Quat Sci,2015,35(2):340-353.
[21] 天津市地球物理勘探中心.天津市平原区1:5万重力调查报告[R].天津:天津市地球物理勘探中心,2008:156-178.
Tianjin Geophysical Exploration Center.1:50,000 gravity survey report in Tianjin Plain area[R].Tianjin:Tianjin Geophysical Exploroction Center,2008:156-178.
[22] 天津市地质矿产局.天津市区域地质志[M].北京:地质出版社,1992:3-142.
Bureau of Geology and Mineral Exploration of Tianjin City.The Regional Geology of Tianjin City[M].Beijing:Geological Publishing House,1992:116-216.
[23] Reimer P J,Bard E,Bayliss A,et al.IntCal13 and Marine13 radiocarbon age calibration curves 0-50 000 years cal BP[J].Radiocarbon,2013,55(4):1869-1887.
[24] 王福,陈永胜,李建芬,等.AMS ¹⁴C测年揭示的渤海湾沿海低地第Ⅱ海相层年龄[J].地质通报,2014,33(10):1591-1595.
Wang F,Chen Y S,Li J F,et al.The age of the second marine layer in coastal lowland of Bohai Bay revealed by AMS ¹⁴C dating method[J].Geol Bull China,2014,33(10):1591-1595.
[25] 商志文,王福,李建芬,等.AMS ¹⁴C测年揭示的渤海湾沿海低地第Ⅱ海相层年龄(Ⅱ)[J].地质通报,2016,35(10):1607-1613.
Shang Z W,Wang F,Li J F,et al.The age of the second marine layer in coastal lowland of Bohai Bay revealed by AMS ¹⁴C dating method (Ⅱ)[J].Geol Bull China,2016,35(10):1607-1613.
[26] 阎玉忠,王宏,李凤林,等.渤海湾西岸晚更新世沉积的差异性特征[J].第四纪研究,2006,26(3):321-326.
Yan Y Z,Wang H,Li F L,et al.Different depositional processes of boreholes BQ1 and BQ2 in the Late Pleistocene on the west coast of Bohai Bay[J].Quat Sci,2006,26(3):321-326.
[27] 陈宇坤,李振海,邵永新,等.天津地区第四纪年代地层剖面研究[J].地震地质,2008,30(2):383-398.
Chen Y K,Li Z H,Shao Y X,et al.Study on the Quaternary chronostratigraphic section in Tianjin area[J].Seismol Geol,2008,30(2):383-398.
[28] Yi L,Lai Z P,Yu H J,et al.Chronologies of sedimentary changes in the south Bohai Sea,China:constraints from luminescence and radiocarbon dating[J].Boreas,2013,42(2):267-284.
[29] 陈永胜,王福,姜兴钰,等.渤海湾西岸QX02孔Ⅱ海的识别及OSL年龄[J].地质通报,2016,35(10):1600-1606.
Chen Y S,Wang F,Jiang X Y,et al.Identification and OSL ages of the second marine bed in bore-hole QX02 along the western coast of Bohai Bay[J].Geol Bull China,2016,35(10):1600-1606.
[30] 施雅风,于革.40-30 ka B.P.中国暖湿气候和海侵的特征与成因探讨[J].第四纪研究,2003,23(1):1-11.
Shi Y F,Yu G.Warm-humid climate and transgressions during 40-30 ka B.P. and their potential mechanisms[J].Quat Sci,2003,23(1):1-11.