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The Correlation of the Fengninian System, the Chinese Lower Carboniferous, as Based on Coral Zones.

The Correlation of the Fengninian System, the Chinese Lower Carboniferous, as Based on Coral Zones. THE CORRELATION OF THE FENGNINIAN SYSTEM, THE CHINESE LOWER CARBONIFEROIJS, AS BASED ON CORAL ZONES. By C.C. Yü (The Geologica' Inslitule, Academic Sinica) IntroductIon. Distribution of Lower Carboniserons in China. Correlation of the Lower Carbonifetons beds from the different localities of our country. Comparison of Chinese Lower Carboniferous Zones with those of Europe. Description of some Index coinis of the faunal zones. I. INTRODUCTION. Much has been written about the Lower Carboniferous formations of central as well as northern China. Through recent field work and researches we now know that the Lower Carboniferous of former authors was far from being correctly determined and that many true Lower Carboniferous beds have been discovered in different localities. Before we consider the distribution of the Lower Carboniferous and its faunal succession, let us briefly summarize the formerly supposed Lower Carboniferousthe Taiyuan series of North China and the Chihsia formation of Central Chinain order to clear the confusion. The term "Taiyuan (*J%) Series" was created by Dr. Wong and Prof. It consists of marine intercalations in the lower part of the Grabau in 1922. so well-known and widespread in North coal-bearing series, which is It was Frech who first considered it to be http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geologica Sinica (English Edition) Wiley

The Correlation of the Fengninian System, the Chinese Lower Carboniferous, as Based on Coral Zones.

Yü, C. C.
Acta Geologica Sinica (English Edition) , Volume 10 (1) – Mar 1, 1931
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Publisher
Wiley
Copyright
Copyright © 1931 Wiley Subscription Services, Inc., A Wiley Company
ISSN
1000-9515
eISSN
1755-6724
DOI
10.1111/j.1755-6724.1931.mp10001001.x
Publisher site
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Abstract

THE CORRELATION OF THE FENGNINIAN SYSTEM, THE CHINESE LOWER CARBONIFEROIJS, AS BASED ON CORAL ZONES. By C.C. Yü (The Geologica' Inslitule, Academic Sinica) IntroductIon. Distribution of Lower Carboniserons in China. Correlation of the Lower Carbonifetons beds from the different localities of our country. Comparison of Chinese Lower Carboniferous Zones with those of Europe. Description of some Index coinis of the faunal zones. I. INTRODUCTION. Much has been written about the Lower Carboniferous formations of central as well as northern China. Through recent field work and researches we now know that the Lower Carboniferous of former authors was far from being correctly determined and that many true Lower Carboniferous beds have been discovered in different localities. Before we consider the distribution of the Lower Carboniferous and its faunal succession, let us briefly summarize the formerly supposed Lower Carboniferousthe Taiyuan series of North China and the Chihsia formation of Central Chinain order to clear the confusion. The term "Taiyuan (*J%) Series" was created by Dr. Wong and Prof. It consists of marine intercalations in the lower part of the Grabau in 1922. so well-known and widespread in North coal-bearing series, which is It was Frech who first considered it to be

Journal

Acta Geologica Sinica (English Edition) – Wiley

Published: Mar 1, 1931

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