INCISED VALLEY OF LAST GLACIAL MAXIMUM STAGE IN THE DRILLING STRATA ON THE TIANJIN-HEBEI COASTAL PLAIN

WANG Qiang

doi:10.12090/j.issn.1006-6616.2019.25.05.072

Volume 25 Issue 5

Oct. 2019

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WANG Qiang, 2019. INCISED VALLEY OF LAST GLACIAL MAXIMUM STAGE IN THE DRILLING STRATA ON THE TIANJIN-HEBEI COASTAL PLAIN. Journal of Geomechanics, 25 (5): 877-888. DOI: 10.12090/j.issn.1006-6616.2019.25.05.072

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INCISED VALLEY OF LAST GLACIAL MAXIMUM STAGE IN THE DRILLING STRATA ON THE TIANJIN-HEBEI COASTAL PLAIN

doi: 10.12090/j.issn.1006-6616.2019.25.05.072

WANG Qiang^{1, 2
,}

1.
Tianjin Center of Geological Survey, China Geological Survey, Tianjin 300170, China
2.
Key Laboratory of Coast Geo-environment, China Geological Survey, Ministry of Natural Resources, Tianjin 300170, China

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Received: 2019-08-19
Revised: 2019-09-09
Published: 2019-10-31

Abstract

Abstract

This paper reviewed the Prof. J.S. Lee's speech on how the Last Glacial Stage climate affected the environment in 1965, as well as the discovery process of the incised valley of the Last Glacial Maximum(LGM)Stage in the drilling strata on the Tianjin-Hebei coastal plain over 40 years. In the source-to-sink processes, at least since Late Pleistocene the study area had been the palaeo-Huanghe (Yellow) River sedimentary area, and the bottom of incised valley of LGM which had been found at many sites were generally at the depth of 30~32 m, lower than that of 20 m of the common Holocene series in the study area. Compared with the depth of 62 m of LGM incised valley in the Changjiang (Yangtze) River estuary area, the range of LGM incised valley in the study area was not as large as the former and there was no unified large estuary. The farthest LGM incised valley occurred at the north urban area of the Mengcun Hui autonomous county of Hebei Province, 80 km from the present coastline, i.e. the top of the Huanghe(Yellow)River sub-delta lobe in Western Han Dynasty. At the same time, the rapid deposition of Early Holocene happened at some drilling holes. It appears that in the study area, only the tributaries of palaeo-Huanghe (Yellow) River could provide such abundant supply, which partly supported the happening of Early Holocene transgression at some areas.
- Last Glacial Maximum,
- incised valley filling,
- source-to-sink,
- resistance of argillaceous sediments to transgression,
- land-ocean interaction,
- Tianjin-Hebei coastal plain

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INCISED VALLEY OF LAST GLACIAL MAXIMUM STAGE IN THE DRILLING STRATA ON THE TIANJIN-HEBEI COASTAL PLAIN

doi: 10.12090/j.issn.1006-6616.2019.25.05.072

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INCISED VALLEY OF LAST GLACIAL MAXIMUM STAGE IN THE DRILLING STRATA ON THE TIANJIN-HEBEI COASTAL PLAIN

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