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Turbidite facies in an ancient subduction complex: Torlesse terrane, New Zealand

Geo-Marine Letters

By:
and
DOI: 10.1007/BF02462470

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Abstract

The Torlesse terrane of New Zealand is an ancient subduction complex consisting of deformed turbidite-facies rocks. These are mainly thick-bedded sandstone (facies B and C) with subordinate mudstone (facies D and E), comparable to inner- and middle-fan deposits of a submarine fan. Strata were deposited in trench-floor and trench-slope settings that received sandy sediment from slope-cutting submarine canyons. The dominance of sandstone suggests that some mudstone may have been selectively subducted. Construction of a detailed sediment dispersal model is not possible because tectonic deformation has largely destroyed original facies relationships and paleocurrent patterns. ?? 1984 Springer-Verlag New York Inc.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Turbidite facies in an ancient subduction complex: Torlesse terrane, New Zealand
Series title:
Geo-Marine Letters
DOI:
10.1007/BF02462470
Volume
3
Issue:
2-4
Year Published:
1984
Language:
English
Publisher:
Springer-Verlag
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Geo-Marine Letters
First page:
211
Last page:
216