Structural evolution within a subduction-transpression transition zone: The Eastern, Marlborough Fault System, New Zealand

被引：0
|
作者：
Audru, JC
Delteil, J
Cutten, H
机构：
来源：
COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES | 1997年 / 324卷 / 01期
关键词：
New Zealand; Marlborough; coastal block; transpression; strike-slip faulting; basin; neogene;
D O I：
暂无
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
In New Zealand, the onland Marlborough Fault System connects the Hikurangi subduction zone with the Alpine Fault. Within the easternmost part of the system, wrench tectonics commenced in the Middle Miocene with subsidence and depositional basins developing adjacent to the faults. On the Alpine Fault, strike-slip movement began in the Early Miocene. Wrench tectonics thus rapidly extended over the entire Marlborough Fault System.
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页码：41 / 48
页数：8
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