Imperial College London
Alternate

Dr Ian Bastow

Faculty of Engineering, Department of Earth Science & Engineering

Senior Lecturer
 
 
 
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Contact

 

+44 (0)20 7594 2974i.bastow Website

 
 
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Location

 

4.45Royal School of MinesSouth Kensington Campus

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Summary

 

Publications

Citation

BibTex format

@article{Gilligan:2016:10.1002/2016GC006419,
author = {Gilligan, A and Bastow, ID and Darbyshire, FA},
doi = {10.1002/2016GC006419},
journal = {Geochemistry Geophysics Geosystems},
pages = {2421--2433},
title = {Seismological structure of the 1.8 Ga Trans-Hudson Orogen of North America},
url = {http://dx.doi.org/10.1002/2016GC006419},
volume = {17},
year = {2016}
}
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RIS format (EndNote, RefMan)

TY  - JOUR
AB  - Precambrian tectonic processes are debated: what was the nature and scale of orogenic events on the younger, hotter, and more ductile Earth? Northern Hudson Bay records the Paleoproterozoic collision between the Western Churchill and Superior plates—the ∼1.8 Ga Trans-Hudson Orogeny (THO)—and is an ideal locality to study Precambrian tectonic structure. Integrated field, geochronological, and thermobarometric studies suggest that the THO was comparable to the present-day Himalayan-Karakoram-Tibet Orogen (HKTO). However, detailed understanding of the deep crustal architecture of the THO, and how it compares to that of the evolving HKTO, is lacking. The joint inversion of receiver functions and surface wave data provides new Moho depth estimates and shear velocity models for the crust and uppermost mantle of the THO. Most of the Archean crust is relatively thin (∼39 km) and structurally simple, with a sharp Moho; upper-crustal wave speed variations are attributed to postformation events. However, the Quebec-Baffin segment of the THO has a deeper Moho (∼45 km) and a more complex crustal structure. Observations show some similarity to recent models, computed using the same methods, of the HKTO crust. Based on Moho character, present-day crustal thickness, and metamorphic grade, we support the view that southern Baffin Island experienced thickening during the THO of a similar magnitude and width to present-day Tibet. Fast seismic velocities at >10 km below southern Baffin Island may be the result of partial eclogitization of the lower crust during the THO, as is currently thought to be happening in Tibet.
AU  - Gilligan,A
AU  - Bastow,ID
AU  - Darbyshire,FA
DO  - 10.1002/2016GC006419
EP  - 2433
PY  - 2016///
SN  - 1525-2027
SP  - 2421
TI  - Seismological structure of the 1.8 Ga Trans-Hudson Orogen of North America
T2  - Geochemistry Geophysics Geosystems
UR  - http://dx.doi.org/10.1002/2016GC006419
UR  - http://hdl.handle.net/10044/1/33260
VL  - 17
ER  -
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