THE VENING-MEINESZ FRACTURE-ZONE AND THE NORTHERN NEW-ZEALAND CONTINENTAL-MARGIN - NEW MORPHOSTRUCTURAL DATA

被引：0
作者：
MASCLE, J
HERZER, R
BASILE, C
机构：
[1] UNIV GRENOBLE 1,INST DOLOMIEU,F-38031 GRENOBLE,FRANCE
[2] INST GEOL & NUCL SCI,LOWER HUTT,NEW ZEALAND
来源：
COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II | 1994年 / 319卷 / 12期
关键词：
CONTINENTAL MARGIN; TRANSFORM BORDER; MORPHOSTRUCTURE; NEW-ZEALAND;
D O I：
暂无
中图分类号：
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号：
07 ; 0710 ; 09 ;
摘要：
A working transit of the Atalante (TRANSNOR, October 1993) has furnished a detailed bathymetric swath showing the morphostructure of the continental slope NW of New Zealand between 168-degrees-40' and 170-degrees-20' East. The remarkable linearity, the steepness of the slope and the presence of a long detached block oriented parallel to the margin, lead us to interpret this sector (with the aid of seismic profiles) as a segment of the Vening Meinesz Fracture Zone that was active locally in the Early Miocene during the geodynamic evolution of this part of the SW Pacific.
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页码：1555 / 1562
页数：8
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