SEDIMENTARY CHARACTERISTICS AND ENVIRONMENT EVOLUTION OF THE HOLOCENE ON THE WEST BANK OF BOHAI BAY

LU Qingwei; SHI Wenxue; GUO Wei; ZHAN Jian; LI Wen

doi:10.16562/j.cnki.0256-1492.2017.01.007

2017 Vol. 37, No. 1

Article Contents

Article navigation > Marine Geology & Quaternary Geology > 2017 > 37(1): 59-66

Next Article Previous Article

LU Qingwei, SHI Wenxue, GUO Wei, ZHAN Jian, LI Wen. SEDIMENTARY CHARACTERISTICS AND ENVIRONMENT EVOLUTION OF THE HOLOCENE ON THE WEST BANK OF BOHAI BAY[J]. Marine Geology & Quaternary Geology, 2017, 37(1): 59-66. doi: 10.16562/j.cnki.0256-1492.2017.01.007

Citation:

LU Qingwei, SHI Wenxue, GUO Wei, ZHAN Jian, LI Wen. SEDIMENTARY CHARACTERISTICS AND ENVIRONMENT EVOLUTION OF THE HOLOCENE ON THE WEST BANK OF BOHAI BAY[J]. Marine Geology & Quaternary Geology, 2017, 37(1): 59-66. doi: 10.16562/j.cnki.0256-1492.2017.01.007

SEDIMENTARY CHARACTERISTICS AND ENVIRONMENT EVOLUTION OF THE HOLOCENE ON THE WEST BANK OF BOHAI BAY

1.
Geological Institute of North China Geological Exploration Bureau of Tianjin, Tianjin 300170
2.
Marine Geological Survey Center of Tianjin, Tianjin 300170

Received Date: 28 June 2016

Revised Date: 08 October 2016

Publish Date: 28 February 2017

Abstract

Abstract

22 drilling holes and 47 scarp profiles were collected from the West Bank of the Bohai Sea for study of characteristics, distribution pattern and depositional environment of the Holocene. The Holocene in the area consists of unconsolidated terrestrial, marine and transitional deposits in various origin, such as alluvial, lacustrine and marine sediments. Upon the influence of sea level changes and tectonic movement, the sediments moved spatially with time and formed 3 wedge-like patterns in the region. Vertically, the sediments usually show fining-up rhythms with local reversed rhythms resulted from sea level variation.
- environmental evolution /
- sedimentary characteristics /
- Tianjin /
- Bohai Bay /
- Holocene

FullText(HTML)

References

[1]	天津市地质矿产局.天津市区域地质志[M].北京:地质出版社, 1992:139-152. Google Scholar Bureau of Geology and Mineral Exploration of Tianjin City. The regional geology of Tianjin City[M]. Beijing: Geological Publishing House, 1992:139-152. Google Scholar
[2]	陈望和, 倪明云, 等.河北第四纪地质[M].北京:地质出版社, 1987:76-173. Google Scholar CHEN Wanghe, NI Mingyun, et al. Hebei Quaternary Geology[M].Beijing: Geological Press, 1987:76-173. Google Scholar
[3]	全国地层委员会编.中国地层指南及中国地层指南说明书[M].北京:地质出版社, 2001. Google Scholar The National Commission on Stratigraphy. Stratigraphic Guide of China and China Stratigraphic Guide Manual[M].Beijing:Geological Press, 2001. Google Scholar
[4]	王宏.渤海湾泥质海岸带近现代地质环境变化研究(Ⅱ):成果与讨论[J].第四纪研究, 2003, 23(4):393-403. doi: 10.3321/j.issn:1001-7410.2003.04.008 CrossRef Google Scholar WANG Hong. Geoenvironmental changes on the Bohai Bay muddy coast (Ⅱ): results and discussions[J]. Quaternary Sciences, 2003, 23(4): 393-403. doi: 10.3321/j.issn:1001-7410.2003.04.008 CrossRef Google Scholar
[5]	王强, 刘立军, 王卫东, 等.环渤海地区及华北平原第四纪古环境变迁机制[J].地质调查与研究, 2006, 27(3):129-138. Google Scholar WANG Qiang, LIU Lijun, WANG Weidong, et al. The mechanism of Quaternary palaeoenvironmental change in circum-Bohai sea region and North China Plain[J].Geological Survey and Research, 2006, 27(3): 129-138. Google Scholar
[6]	王强, 吕金福.海面变化与海岸变迁[C]//中国北方沿海泥炭与环境.北京: 海洋出版社, 1995: 109-128. Google Scholar WANG Qiang, LV Jinfu.Sea change and coastal change[C]// Coastal Peat and the Environment of North China. Beijing: Marine Press, 1995: 109-128. Google Scholar
[7]	李利波, 翟子梅, 周志勇, 等.天津地区黄骅坳陷全新世沉积环境极其变化特征[J].地层学杂志, 2009, 33(4):420-423. doi: 10.3969/j.issn.0253-4959.2009.04.010 CrossRef Google Scholar LI Libo, ZHAI Zimei, ZHOU Zhiyong, et al. Holocene sedimentary environment variation characteristics in huanghua depression area of Tianjin[J].Journal of Stratigraphy, 2009, 33(4):420-423. doi: 10.3969/j.issn.0253-4959.2009.04.010 CrossRef Google Scholar
[8]	吴忱, 魏福利.华北地区晚全新世初期环境变化分析[J].地理与地理信息科学, 2003, 19(2):97-101. doi: 10.3969/j.issn.1672-0504.2003.02.024 CrossRef Google Scholar WU Chen, WEI Fuli. Late Holocene environmental change analysis in north China[J]. Geography and Geoinformation Science, 2003, 19(2):97-101. doi: 10.3969/j.issn.1672-0504.2003.02.024 CrossRef Google Scholar
[9]	尹凤娟, 华洪, 张子福.渤海湾牡蛎礁平原中部兴坨剖面全新世地质环境变迁[J].地质通报, 2004, 23(2):169-176. doi: 10.3969/j.issn.1671-2552.2004.02.011 CrossRef Google Scholar YIN Fengjuan, HUA Hong, ZHANG Zifu.Bohai bay oyster reefs in central plains xingtuo profile Holocene geological environment change[J].Geological Bulletin of China, 2004, 23(2):169-176. doi: 10.3969/j.issn.1671-2552.2004.02.011 CrossRef Google Scholar
[10]	徐馨, 沈志达.全新世环境—最近一万多年来环境变迁[M].贵阳.贵州人民出版社, 1990: 233-235. Google Scholar XU Xin, SHEN Zhida. The Holocene environment——environmental changes in recent ten thousand years[J]. Guiyang: Guizhou People Press, 1990: 233-235. Google Scholar
[11]	赵长荣, Hus J, 阎玉忠, 等.渤海湾西岸晚更新世-全新世年代地层序列与地磁极漂移[J].地质调查与研究, 2003.26(3):183-192. doi: 10.3969/j.issn.1672-4135.2003.03.008 CrossRef Google Scholar ZHAO Changrong, Hus J, YAN Yuzhong, et al. Late Pleistocene-Holocene stratigraphic sequence and geomagnetic pole drift in Bohai bay west bank[J]. Geological Survey and Research, 2003, 26(3):183-192. doi: 10.3969/j.issn.1672-4135.2003.03.008 CrossRef Google Scholar
[12]	王云生, 王宏, 张玉发, 等.泥质海岸带区域地质调查新方法——浅表地层沉积序列法[J].北京:地质出版社, 2003:174-183. Google Scholar WANG Yunsheng, WANG Hong, ZHANG Yufa, Muddy coastal zone new method for regional geological survey, shallow strata sedimentary sequence method[J]. Beijing: Geological Press, 2003:174-183. Google Scholar
[13]	地质矿产部直属单位管理局.沉积岩区1:5万区域地质填图方法指南[M].北京:中国地质大学出版社, 1991. Google Scholar The Geological and Mineral Administration of Directly Affiliated Institutions. 1:50000 Regional Geological Mapping Method Guide of Sedimentary Rock Area[M]. Beijing:China University of Geosciences Press, 1991. Google Scholar
[14]	刘宝珺, 曾允孚.岩相古地理基础和工作方法[M].北京:地质出版社, 1985:120-175. Google Scholar LIU Baojun, ZENG Yunfu. The lithofacies palaeogeographic basis and working methods[M]. Beijing: Geological Press, 1985:120-175. Google Scholar
[15]	商志文, 王宏, 李效广.渤海湾西岸南大港、北大港中晚全新世澙湖底板虚拟重建[J].地质通报, 2005, 27(7):672-676. doi: 10.3969/j.issn.1671-2552.2005.07.014 CrossRef Google Scholar SHANG Zhiwen, WANG Hong, LI Xiaoguang. Middle-late Holocene lake bottom virtual reconstruction in Nandagang and Beidagang, in the west bank of Bohai bay[J]. Geological Bulletin of China, 2005, 27(7):672-676. doi: 10.3969/j.issn.1671-2552.2005.07.014 CrossRef Google Scholar
[16]	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. Google Scholar WANG Pinxian, MIN Qiubao, BIAN Yunhua, et al. The preliminary research on the China Eastern Quaternary transgressive formation[J]. Acta Geologica Sinica, 1981, 55(1):1-13. Google Scholar
[17]	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. doi: 10.3321/j.issn:1001-7410.1999.01.012 CrossRef Google Scholar WANG Qiang. The Bohai Sea in the west bank early Holocene basal peat accumulation is a preliminary study on the time domain[J]. Quaternary Sciences, 1999, 19(1):91. doi: 10.3321/j.issn:1001-7410.1999.01.012 CrossRef Google Scholar
[18]	徐海.中国全新世气候变化研究进展[J].地质地球化学, 2001, 29(2):9-16. doi: 10.3969/j.issn.1672-9250.2001.02.002 CrossRef Google Scholar XU Hai. Advance in research on the Holocene climate fluctuations[J]. Geology-Geochemistry, 2001, 29(2):9-16. doi: 10.3969/j.issn.1672-9250.2001.02.002 CrossRef Google Scholar
[19]	刘嘉麒, 等.第四纪的主要气候事件[J].第四纪研究, 2001, 21(3):239-245. doi: 10.3321/j.issn:1001-7410.2001.03.006 CrossRef Google Scholar LIU Jiaqi. The Quaternary major weather events[J]. Quaternary Research, 2001, 21(3):239-245. doi: 10.3321/j.issn:1001-7410.2001.03.006 CrossRef Google Scholar