EVIDENCE FOR CALEDONIAN SINISTRAL STRIKE-SLIP MOTION AND ASSOCIATED FAULT ZONE WEAKENING, OUTER HEBRIDES FAULT ZONE, NW SCOTLAND

被引:26
作者
BUTLER, CA [1 ]
HOLDSWORTH, RE [1 ]
STRACHAN, RA [1 ]
机构
[1] OXFORD BROOKES UNIV,SCH CONSTRUCT & EARTH SCI,DIV GEOL & CARTOG,OXFORD OX3 0BP,ENGLAND
关键词
OUTER HEBRIDES; FAULTS; REACTIVATION; PHYLLONITES;
D O I
10.1144/gsjgs.152.5.0743
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Outer Hebrides Fault Zone is a major ESE-dipping reactivated fault within the Lewisian gneisses of the Laurentian craton in NW Scotland. Early thrust structures are overprinted by a network of retrograde ductile shear zones in which fluid channelling has hydrated the pre-existing basement rocks at low temperatures, forming chlorite-white mica phyllonites in regions of highest strain. Strike-parallel mineral lineations and shear-sense indicators suggest sinistral displacements that are thought to be late Caledonian based on isotopic data and regional considerations. The phyllonites have focused extensional movements that overprint strike-slip fabrics and may control the location of the Mesozoic Sea of Hebrides and Minch basins.
引用
收藏
页码:743 / 746
页数:4
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