EurekaMag.com logo
+ Site Statistics
References:
53,214,146
Abstracts:
29,074,682
+ Search Articles
+ Subscribe to Site Feeds
EurekaMag Most Shared ContentMost Shared
EurekaMag PDF Full Text ContentPDF Full Text
+ PDF Full Text
Request PDF Full TextRequest PDF Full Text
+ Follow Us
Follow on FacebookFollow on Facebook
Follow on TwitterFollow on Twitter
Follow on Google+Follow on Google+
Follow on LinkedInFollow on LinkedIn

+ Translate

E-MORB- and OIB-type metabasalts from the Karakaya Complex; trace element evidence from melting across the spinel-garnet transition


Eos, Transactions, American Geophysical Union 89.53, Suppl.
E-MORB- and OIB-type metabasalts from the Karakaya Complex; trace element evidence from melting across the spinel-garnet transition

(PDF 0-2 workdays service: $29.90)

Accession: 037038290



Related references

Kinetic inhibition of the garnet-spinel phase transition in upwelling mantle peridotite beneath mid-ocean ridges; a plausible but unlikely explanation for MORB garnet-signature. Abstracts with Programs - Geological Society of America 29(6): 89, 1997

Carbonatite metasomatism and melting of the Arabian lithosphere; evidence from oxygen isotopes and trace element composition of spinel lherzolites. Mineralogical Magazine 58A(A-K): 167-168, 1994

Spinel+ or -garnet lherzolite xenoliths from Pali Aike; Part 2, Trace element and isotopic evidence bearing on the evolution of lithospheric mantle beneath southern Patagonia. Proceedings of the International Kimberlite Conference 7, Vol, 1999

Melting of mantle peridotite at pressures approaching the spinel to garnet transition. Mineralogical Magazine 58A(A-K): 483-484, 1994

Melting in the sub-arc mantle; the effects of H (sub 2) O on primary magmas and the spinel-to-garnet transition. Mineralogical Magazine: A-K, Pages 301-302. 1994., 1994

The Yankan accretion complex as an example of spatial combination of OIB, BABB, N-MORB type metabasalts. International Geological Congress, Abstracts = Congres Geologique International, Resumes 31: (unpaginated, 2000

Experimental constraints on trace element partitioning during dehydration and melting of K-free MORB at 4-6 GPa and 700-1200 OC. Eos, Transactions, American Geophysical Union 89.53, Suppl., 2008

Disequilibrium trace element redistribution during garnet to spinel facies transformation. Proceedings of the International Kimberlite Conference 7, Vol, 1999

Kinetics of garnet to spinel facies transformation and trace element re-distribution. Eos, Transactions, American Geophysical Union: 6, Suppl., Pages 835. 1997., 1997

Melting of mantle peridotite at pressures approaching the spinel to garnet transition; application to mid-ocean ridge basalt petrogenesis. Journal of Geophysical Research: Solid Earth 102(B1): 853-874, 1997