The crustal structure of the Southern Nain and Makkovik Provinces of Labrador deriverd from seismic refraction data.

Research output: Contribution to journal › Journal article › Research › peer-review

Standard

The crustal structure of the Southern Nain and Makkovik Provinces of Labrador deriverd from seismic refraction data. / Funck, T.; Hansen, A.K.; Reid, Ian Derry; Louden, K.E.

In: Canadian Journal of Earth Sciences, Vol. 45, 2008, p. 465-481.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

Funck, T, Hansen, AK, Reid, ID & Louden, KE 2008, 'The crustal structure of the Southern Nain and Makkovik Provinces of Labrador deriverd from seismic refraction data.', Canadian Journal of Earth Sciences, vol. 45, pp. 465-481. <http://rparticle.web-p.cisti.nrc.ca/rparticle/AbstractTemplateServlet?calyLang=eng&journal=cjes&volume=45&year=0&issue=4&msno=e08-007>

APA

Funck, T., Hansen, A. K., Reid, I. D., & Louden, K. E. (2008). The crustal structure of the Southern Nain and Makkovik Provinces of Labrador deriverd from seismic refraction data. Canadian Journal of Earth Sciences, 45, 465-481. http://rparticle.web-p.cisti.nrc.ca/rparticle/AbstractTemplateServlet?calyLang=eng&journal=cjes&volume=45&year=0&issue=4&msno=e08-007

Vancouver

Funck T, Hansen AK, Reid ID, Louden KE. The crustal structure of the Southern Nain and Makkovik Provinces of Labrador deriverd from seismic refraction data. Canadian Journal of Earth Sciences. 2008;45:465-481.

Author

Funck, T. ; Hansen, A.K. ; Reid, Ian Derry ; Louden, K.E. / The crustal structure of the Southern Nain and Makkovik Provinces of Labrador deriverd from seismic refraction data. In: Canadian Journal of Earth Sciences. 2008 ; Vol. 45. pp. 465-481.

Bibtex

@article{fe09d480caa311dd9473000ea68e967b,
title = "The crustal structure of the Southern Nain and Makkovik Provinces of Labrador deriverd from seismic refraction data.",
abstract = "A refraction seismic profile was used to determine the crustal structure across the Nain/ Makkovik boundary, and to look for an offshore continuation of the  Nain Plutonic Suite (NPS). Velocity models were developed from forward and inverse modeling of travel times. There are. In the Saglek block the crust has P-wave velocity 5.8 -6.9 km/s. Further south, upper crustal velocities iand the Poisson's ratio increase. This zone correlates with a gravity low interpreted as the NPS. The upper crustal velocities are compatible with the  NPS. There is a  lower crustal reflector under the NPS. In the Makkovik Province, upper crustal velocities are 5.9-6.2 km/s.. Moho is between 28 and 36 km. The variations may relate to Labrador Sea rifting.",
keywords = "Faculty of Science, Labrador, offshore, seismic, crustal structure",
author = "T. Funck and A.K. Hansen and Reid, {Ian Derry} and K.E. Louden",
year = "2008",
language = "English",
volume = "45",
pages = "465--481",
journal = "Canadian Journal of Earth Sciences",
issn = "0008-4077",
publisher = "N R C Research Press",

}

RIS

TY - JOUR

T1 - The crustal structure of the Southern Nain and Makkovik Provinces of Labrador deriverd from seismic refraction data.

AU - Funck, T.

AU - Hansen, A.K.

AU - Reid, Ian Derry

AU - Louden, K.E.

PY - 2008

Y1 - 2008

N2 - A refraction seismic profile was used to determine the crustal structure across the Nain/ Makkovik boundary, and to look for an offshore continuation of the  Nain Plutonic Suite (NPS). Velocity models were developed from forward and inverse modeling of travel times. There are. In the Saglek block the crust has P-wave velocity 5.8 -6.9 km/s. Further south, upper crustal velocities iand the Poisson's ratio increase. This zone correlates with a gravity low interpreted as the NPS. The upper crustal velocities are compatible with the  NPS. There is a  lower crustal reflector under the NPS. In the Makkovik Province, upper crustal velocities are 5.9-6.2 km/s.. Moho is between 28 and 36 km. The variations may relate to Labrador Sea rifting.

AB - A refraction seismic profile was used to determine the crustal structure across the Nain/ Makkovik boundary, and to look for an offshore continuation of the  Nain Plutonic Suite (NPS). Velocity models were developed from forward and inverse modeling of travel times. There are. In the Saglek block the crust has P-wave velocity 5.8 -6.9 km/s. Further south, upper crustal velocities iand the Poisson's ratio increase. This zone correlates with a gravity low interpreted as the NPS. The upper crustal velocities are compatible with the  NPS. There is a  lower crustal reflector under the NPS. In the Makkovik Province, upper crustal velocities are 5.9-6.2 km/s.. Moho is between 28 and 36 km. The variations may relate to Labrador Sea rifting.

KW - Faculty of Science

KW - Labrador

KW - offshore

KW - seismic

KW - crustal structure

M3 - Journal article

VL - 45

SP - 465

EP - 481

JO - Canadian Journal of Earth Sciences

JF - Canadian Journal of Earth Sciences

SN - 0008-4077

ER -

ID: 9150506