珠江口小榄镇—万顷沙地区晚更新世以来的海侵层序

doi:10.7605/gdlxb.2014.06.067

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Abstract Based on AMS(accelerator mass spectrometry)¹⁴C dating data,analysis of microfossils(foraminifera, ostracoda,diatom),identification of marine bivalve and gastropoda,characteristics of sediment structures and color at the core materials from three standard drilling holes in Zhongshan area,Guangdong Province,combining with the study result of the borehole in adjacent Wanqingsha area,this paper noticed that these four drilling holes, located by E-W direction from the Xiaolan Town to Wanqingsha area, represent the interstream and incised-valley palaeogeographic units at LGM(last glacial maximum) in the Zhujiang River estuary area. Since 9 ka BP(¹⁴C cal age), the incised-valley, which was located in a more restricted sedimentary setting, started to accept the mud sediment, and this is different from in the cutting valley in Changjiang River Delta area and northern China coastal plain where occurred the sandy sediments. At about 7 cal ka BP, the maximum transgression occurred, and transgressive onlap happened upon the LGM weathered layer at interstream area,subsequently the delta formed. According to the correspondence relation between riverine sequence and sea level change,the complete river cycle in which no marine microfossil occurred should be correlated to MIS(marine isotope stage)3 transgression. Based on the buried terrance,and the dating technology cannot make a breakthrough for this segment since over 30 years ago,this paper would consider that there is such a possibility that the regional second thick rich-alluvirum red weathered layer from top to bottom would be sediments of the lowstand system tract of MIS4,and the lowest estuarine sedimentary unit which is rich in organic matter, and in which a few marine bivalves and gastropoda shells can be found, would be belonged to sediments of late MIS5.

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	Articles by authors
	Xie Yecai
	Wang Qiang
	Long Gui
	Zhou Yang
	Zheng Zhimin
	Huang Xuefei

Key words： Zhujiang River estuary MIS3 transgressive sequence incised valley transgressive onlap stratigraphic architecture

Received: 07 March 2014 Published: 01 December 2014

ZTFLH:

P534.63

About author: Xie Yecai,born in 1977,is a senior engineer of Quaternary geology at Guangdong Geologic Survey Institute. E-mail: xieyecai@foxmail.com.
About the corresponding author Wang Qiang,born in 1945,is a professor of Quaternary geology and marine geology at Tianjin Institute of Geology and Mineral Resources. E-mail: tjwq1945@163.com.

Cite this article:

Xie Yecai,Wang Qiang,Long Gui et al. Transgressive sequence since the Late Pleistocene in Xiaolan Town-Wanqingsha area, Zhujiang River estuary[J]. JOPC, 2014, 16(6): 835-852.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2014.06.067 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2014/V16/I6/835

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