哈尔滨荒山剖面第四纪地层研究

王永; 董进; 杨劲松

doi:10.3799/dqkx.2020.171

Volume 45 Issue 7

Jul. 2020

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Wang Yong, Dong Jin, Yang Jingsong, 2020. Quaternary Stratigraphy of the Huangshan Section in Harbin. Earth Science, 45(7): 2662-2672. doi: 10.3799/dqkx.2020.171

Citation:

Wang Yong, Dong Jin, Yang Jingsong, 2020. Quaternary Stratigraphy of the Huangshan Section in Harbin. Earth Science, 45(7): 2662-2672. doi: 10.3799/dqkx.2020.171

Wang Yong, Dong Jin, Yang Jingsong, 2020. Quaternary Stratigraphy of the Huangshan Section in Harbin. Earth Science, 45(7): 2662-2672. doi: 10.3799/dqkx.2020.171

Citation:

Wang Yong, Dong Jin, Yang Jingsong, 2020. Quaternary Stratigraphy of the Huangshan Section in Harbin. Earth Science, 45(7): 2662-2672. doi: 10.3799/dqkx.2020.171

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Quaternary Stratigraphy of the Huangshan Section in Harbin

doi: 10.3799/dqkx.2020.171

Wang Yong^{1
,
,},
Dong Jin¹,
Yang Jingsong^{2, 3}

1.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijianzhuan 050061, China
3.
Key Laboratory of Quaternary Chronology and Hydro-Environmental Evolution, Chinese Academy of Geological Sciences, Shijianzhuang 050061, China

Received Date: 2020-06-23
Publish Date: 2020-07-15

Abstract

Abstract

The Huangshan section in Harbin is considered as a standard Quaternary sedimentary sequence for terrestrial strata in Northeast China. Due to the lack of absolute age data, there are different results about its stratigraphic division and the chronostratigraphy. In this paper, a detailed magnetostratigraphic investigation, coupled with AMS¹⁴C, OSL and other chronological data was carried out on the Huangshan section. The chronological framework of Quaternary strata of the Huangshan section is redefined. The results show that the magnetic polarity stratigraphy includes late Matuyama negative polarity chron to Brunhes positive polarity chron in the Huangshan section. The B/M boundary is at 46.7 m in lower part of the section, and the initial deposition age of the section is earlier than 0.90 Ma. The Holocene and Upper Pleistocene lower boundaries are determined according to AMS¹⁴C and OSL ages. The sequence of Huangshan section comprises in chronological order the Xiahuangshan, Shanghuangshan, Harbin, Guxiangtun and Tantu Formations. The age of each lithostratigraphic unit in the Quaternary is determined as follows:the Xiahuangshan Formation is deposited earlier than 900 ka BP; the age of the Shanghuangshan Formation is 138-580 ka BP, that of the Harbin Formation is 79-138 ka BP, that of the Guxiangtun Formation is 12-79 ka BP, and the age of the Tantu Formation is~12 ka BP. The results provide new data for the Quaternary stratigraphic system of Huangshan section, and the division and correlation of Quaternary strata in Northeast China.
- Harbin,
- Huangshan section,
- Quaternary,
- magnetostratigraphy,
- chronostratigraphy,
- stratigraphy

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References(60)

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