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Some Devonian Fossils From Kweilin and Other Localities in Kwangsi*

Some Devonian Fossils From Kweilin and Other Localities in Kwangsi* BULLETIN OF THE GEOLOGLCAL SOCIETY OF CHINA vot.. xxvii. ii. 123-140, 3 vis. NOVEMBER 1947 Some Devonian Fos!ls From Kweilin and Other Localities in Kwangsi C. C. Yü (Institute of Geology, Academia Sinica With 3 Plates The city of Kweilin is surrounded by the hills which are entirely composed The limestones may be classified into two of limestones of the Devonian age. less crystalline groups. The lower one is the thinly bedded, dark gray, more or x- dolomitic limestone attaining a thickness of about 80 meters with the base not posed, while the upper part as observed at Hou-shan (ii) and Tzi-hsun-yen consists of whitish gray or grayish white thick-bedded limestone, being scarcely yielded any remains more than 100 meters thick. The upper limestone has of ancient organisms, but in the lower group nothing can be found more than the form Amphipora which occurs in many beds at Lao-jen-shan (Ailj ) and appeirs Although the Rugose corals are hardly found in to be the reef-builder then. such thick limestone beds as these in the neighbourhood of Kweilin, the writer, however, has fortunately collected at Liu-ma-shan (.ili) some well-preserved As its specimens of Disphylium liumacase (n. sp.) from the lower http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geologica Sinica (English Edition) Wiley

Some Devonian Fossils From Kweilin and Other Localities in Kwangsi*

Acta Geologica Sinica (English Edition) , Volume 27 (1) – Mar 1, 1947

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Publisher
Wiley
Copyright
Copyright © 1947 Wiley Subscription Services, Inc., A Wiley Company
ISSN
1000-9515
eISSN
1755-6724
DOI
10.1111/j.1755-6724.1947.mp27001010.x
Publisher site
See Article on Publisher Site

Abstract

BULLETIN OF THE GEOLOGLCAL SOCIETY OF CHINA vot.. xxvii. ii. 123-140, 3 vis. NOVEMBER 1947 Some Devonian Fos!ls From Kweilin and Other Localities in Kwangsi C. C. Yü (Institute of Geology, Academia Sinica With 3 Plates The city of Kweilin is surrounded by the hills which are entirely composed The limestones may be classified into two of limestones of the Devonian age. less crystalline groups. The lower one is the thinly bedded, dark gray, more or x- dolomitic limestone attaining a thickness of about 80 meters with the base not posed, while the upper part as observed at Hou-shan (ii) and Tzi-hsun-yen consists of whitish gray or grayish white thick-bedded limestone, being scarcely yielded any remains more than 100 meters thick. The upper limestone has of ancient organisms, but in the lower group nothing can be found more than the form Amphipora which occurs in many beds at Lao-jen-shan (Ailj ) and appeirs Although the Rugose corals are hardly found in to be the reef-builder then. such thick limestone beds as these in the neighbourhood of Kweilin, the writer, however, has fortunately collected at Liu-ma-shan (.ili) some well-preserved As its specimens of Disphylium liumacase (n. sp.) from the lower

Journal

Acta Geologica Sinica (English Edition)Wiley

Published: Mar 1, 1947

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