Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Scott A. Barboza"'
Autor:
Scott A. Barboza, George W. Bergantz
Publikováno v:
Journal of Petrology. 41:1307-1327
Emplacement of mantle-derived magma (magmatic accretion) is the total thermal budget of the continental lower crust, often presumed or inferred to be an important cause of regional produce regional granulite facies metamorphism, and granulite facies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::13ca64cdaaf204af8d0357be4845a35a
https://doi.org/10.1093/petrology/41.8.1307
https://doi.org/10.1093/petrology/41.8.1307
Autor:
Scott A. Barboza, George W. Bergantz
Publikováno v:
Earth and Planetary Science Letters. 158:19-29
High-grade igneous and metamorphic systems which possess a variable percentage of melt, may undergo a transition between crystal-supported and fully fluid behavior. The melt-fraction interval over which this transition occurs is not well constrained.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::678936a65adbcc277226e4c3afa2355e
https://doi.org/10.1016/s0012-821x(98)00047-8
https://doi.org/10.1016/s0012-821x(98)00047-8
Autor:
Scott A. Barboza, George W. Bergantz
Publikováno v:
Numerical Heat Transfer, Part A: Applications. 31:375-392
The binary-eutectic model of phase change limits the application of continuum-mixture simulations to particular systems. The authors present a phase-change model that allows systems with more complex phase relations to be addressed. The model include
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fad786759d8d303e4081ba5d0180308b
https://doi.org/10.1080/10407789708914043
https://doi.org/10.1080/10407789708914043
Rock ejecta brought to the surface by mud volcanoes offer a unique opportunity to characterize sedimentary units both within and beyond conventional drilling depths. Present among ejecta from mud volcanoes in the South Caspian Basin are the organic-r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8e52320407b78275e800ea84769a42b
https://doi.org/10.1306/1205839st551436
https://doi.org/10.1306/1205839st551436
Autor:
Scott A. Barboza
Publikováno v:
Geofluids. 7:272-273
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d8a545fa89dac687c46a2a81e640cbaf
https://doi.org/10.1111/j.1468-8123.2007.00174.x
https://doi.org/10.1111/j.1468-8123.2007.00174.x
Autor:
Scott A. Barboza, George W. Bergantz
Dehydration melting of crustal rocks may commonly occur in response to the intrusion of mafic magma in the mid- or lower crust. However, the relative importance of melt buoyancy, shear or dyking in melt generation and extraction under geologically re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63af84edf5c114041d3a98f112a8652f
https://doi.org/10.1130/0-8137-2315-9.23
https://doi.org/10.1130/0-8137-2315-9.23
Publikováno v:
Geology. 27:447
One widely accepted paradigm for the development of continental lower crust is that regional granulite facies metamorphism is caused by intrusion of mafic magma beneath or into the crust (magmatic accretion). The amphibolite to granulite facies supra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eea329e5defbefed8e0274226dd76a38
https://doi.org/10.1130/0091-7613(1999)027<0447:rgfmit>2.3.co
https://doi.org/10.1130/0091-7613(1999)027<0447:rgfmit>2.3.co