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Magnetostratigraphy of two deep boreholes in southwestern Bohai Bay: Tectonic implications and constraints on the ages of volcanic layers
Xu, Qinmian1; Yang, Jilong1; Hu, Yunzhuang1; Yuan, Guibang1; Deng, Chenglong2,3
2018-02-01
Source PublicationQUATERNARY GEOCHRONOLOGY
ISSN1871-1014
Volume43Pages:102-114
SubtypeArticle
AbstractThe sediments of Bohai Bay Basin have recorded the processes of basin infilling and structural evolution, reflecting the destruction of the North China Craton during the late Mesozoic and the early Cenozoic. However, the absence of a reliable chronostratigraphic framework for the sedimentary sequences in the basin has precluded a comprehensive understanding of these processes. This is especially the case for southwestern Bohai Bay, the evolution of which has been affected by two Quaternary volcanoes, Dashan and Xiaoshan. In this study, we combine paleomagnetic and sedimentary analyses of the sediments from two boreholes (CK3 and G4) from southwestern Bohai Bay Basin in order to provide new insights into the sedimentary history and regional tectonic processes since the Pliocene. The main findings.are as follows. (1) Magnetite and hematite are the main carriers of the characteristic remanent magnetization in these sedimentary sequences, with hematite the main component. (2) The two drill cores record the Brunhes, Olduvai and Gauss normal chrons, and the Matuyama and Gilbert reverse chrons. (3) Subsidence-related differences in the depths of the Matuyama/Brunhes (MOB) and Gauss/Matuyama (G/M) boundaries in boreholes across Bohai Bay, distributed within different structural units, reflect the fact that northern Bohai Bay is the regional subsidence center and that the development of the WNW-orientated structures of the basin has intensified during the Quaternary. (4) The trend of changes in the elevation of three marine layers is similar to that of the MOB and G/M boundaries across Bohai Bay. Based on magneto-stratigraphic constraints of the boreholes, the ages of the second and third marine layers are assigned to Marine Oxygen Isotope (MIS) 3 and MIS 5, respectively. The WNW-orientated structures and 'super interglacials' resulted in the formation of transgressions in the Huanghua depression. (5) In borehole CK3, the ages of four volcanic layers at the depth intervals of 13.14-16.18 m, 33.37-48.02 m, 145.8 -154.05 m and 222.16-233.80 m, are 10-18 ka BP, 80-90 ka BP, 2.2 Ma and 3.1 Ma, respectively. In borehole G4, the age of the volcanic layer at the depth of 46.4-55.8 m is 0.33-0.55 Ma. Comparative analysis of subsidence-related differences between the NEE and NE-orientated uplifts and depressions in western and southern Bohai Bay indicates that structural evolution in the vertical plane during the Quaternary was mainly controlled by the subduction of the Pacific Plate. (C) 2017 Elsevier B.V. All rights reserved.
KeywordSouthwestern Bohai Bay Late Cenozoic Magnetostratigraphy Volcanic Layers
WOS HeadingsScience & Technology ; Physical Sciences
DOI10.1016/j.quageo.2017.08.006
Funding OrganizationChina Geological Survey Project(12120114007801 ; China Geological Survey Project(12120114007801 ; National Natural Science Foundation of China(41690112 ; National Natural Science Foundation of China(41690112 ; 1212011120170 ; 1212011120170 ; 41621004) ; 41621004) ; 1212011120746 ; 1212011120746 ; 1212010610408 ; 1212010610408 ; DD2016042) ; DD2016042) ; China Geological Survey Project(12120114007801 ; China Geological Survey Project(12120114007801 ; National Natural Science Foundation of China(41690112 ; National Natural Science Foundation of China(41690112 ; 1212011120170 ; 1212011120170 ; 41621004) ; 41621004) ; 1212011120746 ; 1212011120746 ; 1212010610408 ; 1212010610408 ; DD2016042) ; DD2016042) ; China Geological Survey Project(12120114007801 ; China Geological Survey Project(12120114007801 ; National Natural Science Foundation of China(41690112 ; National Natural Science Foundation of China(41690112 ; 1212011120170 ; 1212011120170 ; 41621004) ; 41621004) ; 1212011120746 ; 1212011120746 ; 1212010610408 ; 1212010610408 ; DD2016042) ; DD2016042) ; China Geological Survey Project(12120114007801 ; China Geological Survey Project(12120114007801 ; National Natural Science Foundation of China(41690112 ; National Natural Science Foundation of China(41690112 ; 1212011120170 ; 1212011120170 ; 41621004) ; 41621004) ; 1212011120746 ; 1212011120746 ; 1212010610408 ; 1212010610408 ; DD2016042) ; DD2016042)
WOS KeywordTEMPERATURE-DEPENDENT SUSCEPTIBILITY ; CHINESE LOESS PLATEAU ; SEA-LEVEL CHANGE ; LATE PLEISTOCENE ; NORTH CHINA ; RIVER DELTA ; ACTIVE TECTONICS ; CLIMATE-CHANGE ; LUMINESCENCE ; RECORD
Indexed BySCI
Language英语
Funding OrganizationChina Geological Survey Project(12120114007801 ; China Geological Survey Project(12120114007801 ; National Natural Science Foundation of China(41690112 ; National Natural Science Foundation of China(41690112 ; 1212011120170 ; 1212011120170 ; 41621004) ; 41621004) ; 1212011120746 ; 1212011120746 ; 1212010610408 ; 1212010610408 ; DD2016042) ; DD2016042) ; China Geological Survey Project(12120114007801 ; China Geological Survey Project(12120114007801 ; National Natural Science Foundation of China(41690112 ; National Natural Science Foundation of China(41690112 ; 1212011120170 ; 1212011120170 ; 41621004) ; 41621004) ; 1212011120746 ; 1212011120746 ; 1212010610408 ; 1212010610408 ; DD2016042) ; DD2016042) ; China Geological Survey Project(12120114007801 ; China Geological Survey Project(12120114007801 ; National Natural Science Foundation of China(41690112 ; National Natural Science Foundation of China(41690112 ; 1212011120170 ; 1212011120170 ; 41621004) ; 41621004) ; 1212011120746 ; 1212011120746 ; 1212010610408 ; 1212010610408 ; DD2016042) ; DD2016042) ; China Geological Survey Project(12120114007801 ; China Geological Survey Project(12120114007801 ; National Natural Science Foundation of China(41690112 ; National Natural Science Foundation of China(41690112 ; 1212011120170 ; 1212011120170 ; 41621004) ; 41621004) ; 1212011120746 ; 1212011120746 ; 1212010610408 ; 1212010610408 ; DD2016042) ; DD2016042)
WOS Research AreaPhysical Geography ; Geology
WOS SubjectGeography, Physical ; Geosciences, Multidisciplinary
WOS IDWOS:000418981800009
PublisherELSEVIER SCI LTD
Citation statistics
Cited Times:2[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/93145
Collection岩石圈演化国家重点实验室
Corresponding AuthorXu, Qinmian
Affiliation1.China Geol Survey, Tianjin Ctr, Tianjin 300170, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 10029, Peoples R China
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
Recommended Citation
GB/T 7714
Xu, Qinmian,Yang, Jilong,Hu, Yunzhuang,et al. Magnetostratigraphy of two deep boreholes in southwestern Bohai Bay: Tectonic implications and constraints on the ages of volcanic layers[J]. QUATERNARY GEOCHRONOLOGY,2018,43:102-114.
APA Xu, Qinmian,Yang, Jilong,Hu, Yunzhuang,Yuan, Guibang,&Deng, Chenglong.(2018).Magnetostratigraphy of two deep boreholes in southwestern Bohai Bay: Tectonic implications and constraints on the ages of volcanic layers.QUATERNARY GEOCHRONOLOGY,43,102-114.
MLA Xu, Qinmian,et al."Magnetostratigraphy of two deep boreholes in southwestern Bohai Bay: Tectonic implications and constraints on the ages of volcanic layers".QUATERNARY GEOCHRONOLOGY 43(2018):102-114.
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