EXTINCT MID-OCEAN RIDGES IN TASMAN SEA AND IN WESTERN PACIFIC

被引:22
作者
VANDERLINDEN, WJ
机构
[1] New Zealand Oceanographic Institute, Department of Scientific and Industrial Research, Wellington
关键词
D O I
10.1016/0012-821X(69)90120-4
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Recent magnetic surveys in the Tasman Sea suggest the Dampier Ridge to be an extinct or dormant mid-ocean ridge. The concept of ancient sea-floor spreading activity provides an attractive explanation of the structural evolution of the South West Pacific. The concept may also explain the anomalous position of island arcs and trenches in the Western Pacific. © 1969.
引用
收藏
页码:483 / +
页数:1
相关论文
共 22 条
[1]  
BARAZANGI M, 1969, B SEISMOL SOC AM, V59, P369
[2]   ISLAND ARCS IN THE DEVELOPMENT OF THE EARTHS STRUCTURE (ESPECIALLY IN THE REGION OF JAPAN AND THE SEA OF OKHOTSK) [J].
BELOUSSOV, VV ;
RUDITCH, EM .
JOURNAL OF GEOLOGY, 1961, 69 (06) :647-&
[3]  
BRODIE JW, 1959, GEOL RDSCH, V47, P662
[4]  
BRODIE JW, 1952, NZ J SCI TECH, VB33, P373
[5]   WESTERN TASMAN SEA FLOOR [J].
CONOLLY, JR .
NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS, 1969, 12 (01) :310-&
[6]  
DIETZ RS, 1954, GEOL SOC AM BULL, V65, P1199, DOI 10.1130/0016-7606(1954)65[1199:MGONPD]2.0.CO
[7]  
2
[8]  
EVISON FF, 1968, CAN J EARTH SCI, V5, P1045
[9]  
Hess H. H., 1948, B SOC GEOL AM, V59, P417
[10]  
MENARD HW, 1968, BATHYMETRY SOUTHWEST