Thermal regime of the Costa Rican convergent margin: 1. Along-strike variations in heat flow from probe measurements and estimated from bottom-simulating reflectors-Reference-Cited by-同舟云学术

Thermal regime of the Costa Rican convergent margin: 1. Along-strike variations in heat flow from probe measurements and estimated from bottom-simulating reflectors

Published:2010-12 Issue:12 Volume:11 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Harris Robert N.¹,Grevemeyer Ingo²,Ranero César R.³,Villinger Heinrich⁴,Barckhausen Udo⁵,Henke Thomas,Mueller Christian⁵,Neben Soenke⁵

Affiliation:

1. College of Oceanic and Atmospheric Sciences; Oregon State University; Corvallis; Oregon; 97331; USA

2. Leibniz Institute of Marine Sciences at University of Kiel (IFM-GEOMAR); D-24148; Kiel; Germany

3. Barcelona Center for Subsurface Imaging; ICREA, Instituto de Ciencias del Mar, CSIC; Pg. Marítim de la Barcelona 37-49,; E-08003; Barcelona; Spain

4. Department of Geosciences; University of Bremen; PO Box 330 440 D-28334; Bremen; Germany

5. Federal Institute for Geosciences and Natural Resources; Stilleweg 2,; D-30655; Hannover; Germany

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://www.agu.org/journals/gc/gc1012/2010GC003272/2010GC003272.pdf

Reference59 articles.

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3. Thermal regime of the Chile triple junction: Constraints provided by downhole temperature measurements and distribution of gas hydrate;Brown;Proc. Ocean Drill. Program Initial Rep.,1995

4. Lithium isotopic compositions of pore fluids and sediments in the Costa Rica subduction zone: Implications for fluid processes and sediment contribution to the arc volcanoes;Chan;Earth Planet. Sci. Lett.,2000

5. Structure of the Costa Rica convergent margin, offshore Nicoya Peninsula;Christeson;J. Geophys. Res.,1999

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