关于“大贵州滩”

doi:10.7605/gdlxb.2015.04.047

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Abstract

In 1990s,Lehrmann et al. called the Early Triassic isolated “Luodian Carbonate Platform”in the Luodian area of southern Guizhou Province in South China as the “Great Bank of Guizhou”. This term “Great Bank of Guizhou”was cited in more than 300 articles in foreign countries. The authors of this paper have studied the lithofacies palaeogeography of the Early and Middle Triassic in South China. According to the geological data of us,in the Early Triassic and in the Luodian area of southern Guizhou Province,there was only an isolated “Luodian Carbonate Platform”,but there was no “Great Bank of Guizhou”. The isolated “Luodian Carbonate platform”should not be called as the “Great Bank of Guizhou”.This paper is a detailed abstract of the English article There was no “Great Bank of Guizhou”in the Early Triassic in Guizhou Province,South China(Journal of Palaeogeoraphy(English Edition),2015,4(1)). The aim of this paper is to let Chinese readers understand that the term “Great Bank of Guizhou”did not match the reality seriously and should not be used any more.

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	Feng Zengzhao
	Bao Zhidong
	Zheng Xiujuan
	Wang Yuan

Key words： South China Early Triassic “Great Bank of Guizhou” “Luodian Carbonate Platform” Bianyang section name and reality

Received: 15 May 2015 Published: 01 August 2015

ZTFLH:

P531

About author: Feng Zengzhao,born in 1926,gratuated from the Department of Geology at Tsinghua University in 1952. Now,he is a professor in China University of Petroleum(Beijing)and is engaged in sedimentology and palaeogeography. E-mail:Jpalaeo2012@163.com.

Cite this article:

Feng Zengzhao,Bao Zhidong,Zheng Xiujuan et al. About the “Great Bank of Guizhou”[J]. JOPC, 2015, 17(4): 573-575.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2015.04.047 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2015/V17/I4/573

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