Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Kiara L. Alessio"'
Publikováno v:
Geosciences, Vol 7, Iss 3, p 75 (2017)
Phase equilibria modelling incorporating melt reintegration offers a methodology to create hypothetical rock compositions that may have existed prior to melt loss, allowing the potential prograde evolution of rocks to be explored. However, melt reint
Externí odkaz:
https://doaj.org/article/b7ae366ba60f440b9dfe32174545f70c
Publikováno v:
Lithos. :222-235
The spatial distribution of heat producing elements (K, U, and Th) in the continental crust has long-term implications for the thermal and physical evolution of orogens. Heat producing elements, in particular Th, are most abundant in metasedimentary
Autor:
Karin M. Barovich, Laura J. Morrissey, Martin Hand, Kiara L. Alessio, David E. Kelsey, Megan A. Williams
Publikováno v:
Geology. 46:335-338
Partial melting of continental crust is generally considered to produce granitic rocks that have high radiogenic heat production rates when compared to their inferred sources and average continental crust. If this idea is correct, then granulite-faci
Autor:
David E. Kelsey, Tom Raimondo, Derrick Hasterok, Martin Hand, Kiara L. Alessio, Laura J. Morrissey
Publikováno v:
Lithos. :105280
The Reynolds Range in the Paleo-Mesoproterozoic Aileron Province of central Australia exposes a differentially exhumed metamorphic rock system varying from greenschist-to granulite-facies. Calculated P-T pseudosections indicate that peak metamorphic
Publikováno v:
Geosciences, Vol 7, Iss 3, p 75 (2017)
Geosciences; Volume 7; Issue 3; Pages: 75
Geosciences; Volume 7; Issue 3; Pages: 75
Phase equilibria modelling incorporating melt reintegration offers a methodology to create hypothetical rock compositions that may have existed prior to melt loss, allowing the potential prograde evolution of rocks to be explored. However, melt reint
Autor:
Karin M. Barovich, Laura J. Morrissey, David E. Kelsey, Kiara L. Alessio, Megan A. Williams, Martin Hand
Publikováno v:
Geology. 46:480-480