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Neotectonics of the Owen Fracture Zone (NW Indian Ocean): Structural evolution of an oceanic strike-...

Neotectonics of the Owen Fracture Zone (NW Indian Ocean): Structural evolution of an oceanic strike-...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_00643186v1

Neotectonics of the Owen Fracture Zone (NW Indian Ocean): Structural evolution of an oceanic strike-slip plate boundary

About this item

Full title

Neotectonics of the Owen Fracture Zone (NW Indian Ocean): Structural evolution of an oceanic strike-slip plate boundary

Publisher

Washington: Blackwell Publishing Ltd

Journal title

Geochemistry, geophysics, geosystems : G3, 2011-12, Vol.12 (12), p.1-n/a

Language

English

Formats

Publication information

Publisher

Washington: Blackwell Publishing Ltd

More information

Scope and Contents

Contents

The Owen Fracture Zone is a 800 km‐long fault system that accommodates the dextral strike‐slip motion between India and Arabia plates. Because of slow pelagic sedimentation rates that preserve the seafloor expression of the fault since the Early Pliocene, the fault is clearly observed on bathymetric data. It is made up of a series of fault segments...

Alternative Titles

Full title

Neotectonics of the Owen Fracture Zone (NW Indian Ocean): Structural evolution of an oceanic strike-slip plate boundary

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_hal_primary_oai_HAL_hal_00643186v1

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_00643186v1

Other Identifiers

ISSN

1525-2027

E-ISSN

1525-2027

DOI

10.1029/2011GC003731

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