Your single point of reference for all your Geotechnical Inquiries
No reviews have been submitted for this Publication so far.
You must be registered in order to submit a review.
You must be registered in order to submit a review.
Share this Information:
|
|
|
PHASE TRANSFORMATIONS OF CONTINENTAL CRUST DURING SUBDUCTION AND EXHUMATION: WESTERN GNEISS REGION, NORWAY (2009)
This paper first presents Sm-Nd geochronology that dates garnet growth in quartzofeldspathic gneisses. Second, modeling of compositional zoning in garnet is used to constrain the pressures and temperatures of garnet growth. This paper finally discusses how this conclusion affects our understanding of the density of subducted crust, the global geochemical cycle and the rheology of continental crust.
Reference:
Eur. J. Mineral. 2009, 21, 1097-1118, Published online December 2009
Eur. J. Mineral. 2009, 21, 1097-1118, Published online December 2009
Organization:
Department of Earth Science, University of California, Santa Barbara, Santa Barbara, USA
Norway
Department of Earth Science, University of California, Santa Barbara, Santa Barbara, USA
Norway
User Rating:
You must be registered to vote.
