THE DISCOVERY OF LOWER ORDOVICIAN CONODONTS FROM LINXIAN COUNTY OF HENAN PROVINCE AND BIOSTRATIGRAPHICAL CORRELATION

PEI Fang; CAI Shu-hua

doi:10.12097/gbc.ZQYD198902003

Geological Bulletin of China > 1989 > (2): 27-32. > DOI: 10.12097/gbc.ZQYD198902003

PEI Fang, CAI Shu-hua. 1989: THE DISCOVERY OF LOWER ORDOVICIAN CONODONTS FROM LINXIAN COUNTY OF HENAN PROVINCE AND BIOSTRATIGRAPHICAL CORRELATION. Geological Bulletin of China, (2): 27-32. DOI: 10.12097/gbc.ZQYD198902003

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THE DISCOVERY OF LOWER ORDOVICIAN CONODONTS FROM LINXIAN COUNTY OF HENAN PROVINCE AND BIOSTRATIGRAPHICAL CORRELATION

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Available Online: August 17, 2023
Published Date: May 14, 1989

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The north part of Henan Province is located geologically in the south part of the North China platform,no lower Ordovician fossil was collected in last decades.Recenty,the authors found the lower Ordovician conodonts from Linxian County,thus providing the basis for determation,subdivision and correlation of lower Ordovician in this area. Based on the abundant eonodonts,Yeli and Liangjiaohan Formations can be divided,and“Acodus”oneotensis-Scolopodus restrictus zone in Yeli Formation and Paraserratognathus paltodiformis zone in Liangjiashan Formation can be established in this area. Acorrding to the first discovery of a conglomorate bed in the base of Liangjiashan Formation and the lacuna of several Lower Ordovician conodont zones of North China,a sedimentary hiatus can be determented in this area.

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THE DISCOVERY OF LOWER ORDOVICIAN CONODONTS FROM LINXIAN COUNTY OF HENAN PROVINCE AND BIOSTRATIGRAPHICAL CORRELATION

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