A NEW LOWER ORDOVICIAN CONODONT FAUNULE FROM THE NORTHERN BELT OF THE SOUTHERN UPLANDS

被引:20
作者
ARMSTRONG, HA
CLARKSON, ENK
OWEN, AW
机构
[1] UNIV EDINBURGH,GRANT INST GEOL,EDINBURGH EH9 3JW,MIDLOTHIAN,SCOTLAND
[2] UNIV GLASGOW,DEPT GEOL & APPL GEOL,GLASGOW G12 8QQ,SCOTLAND
关键词
D O I
10.1144/sjg26010047
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
A deep water Periodon-Prioniodus-Protopanderodus assemblage has been isolated from red cherts and mudstones in the Hawkwood Burn, a tributary of the Wandel Burn. Constraints provided by associated graptolites and the absence of Pygodus and Arenig taxa known to occur in the Southern Uplands suggest this part of the sequence is Llanvirn in age. -Authors
引用
收藏
页码:47 / 52
页数:6
相关论文
共 37 条
[31]  
Pringle J., 1948, BRIT REGIONAL GEOLOG, Vsecond
[32]  
REJEBIAN VA, 1987, GEOL SOC AM BULL, V99, P471, DOI 10.1130/0016-7606(1987)99<471:CCATAA>2.0.CO
[33]  
2
[34]  
SMITH J, 1907, T NATURAL HIST SOC G, V7, P235
[35]   A SEQUENTIAL BACK-ARC AND FORELAND BASIN THRUST DUPLEX MODEL FOR THE SOUTHERN UPLANDS OF SCOTLAND [J].
STONE, P ;
FLOYD, JD ;
BARNES, RP ;
LINTERN, BC .
JOURNAL OF THE GEOLOGICAL SOCIETY, 1987, 144 :753-764
[36]  
SWEET WC, 1984, PALAEONTOLOGICAL CON, V295, P23
[37]  
TIPNIS RS, 1978, 781C GEOL SURV CAN P, P75