Zobrazeno 1 - 10
of 124
pro vyhledávání: '"B. Ronald Frost"'
Publikováno v:
Laurentia: Turning Points in the Evolution of a Continent ISBN: 9780813712208
The Archean Wyoming Province formed and subsequently grew through a combination of magmatic and tectonic processes from ca. 4.0 to 2.5 Ga. Turning points in crustal evolution are recorded in four distinct phases of magmatism: (1) Early mafic magmatis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b5e713dfea875fff3be6aba9f246ce96
https://doi.org/10.1130/2022.1220(01)
https://doi.org/10.1130/2022.1220(01)
Autor:
Carol D. Frost, B. Ronald Frost
Publikováno v:
Laurentia: Turning Points in the Evolution of a Continent ISBN: 9780813712208
Ferroan granite is a characteristic rock type of the Laurentian margin. It is commonly associated with anorthosite and related rocks. Ferroan granites are strongly enriched in iron, are alkalic to alkali-calcic, and are generally metaluminous. These
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ebb44b2b54005fa0ee5c2fff362619e5
https://doi.org/10.1130/2022.1220(10)
https://doi.org/10.1130/2022.1220(10)
Autor:
Carol D. Frost, B. Ronald Frost
Publikováno v:
Essentials of Igneous and Metamorphic Petrology. :293-314
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::57fec7400eca2c5ef43b4a536d1ab85e
https://doi.org/10.1017/9781108685047.021
https://doi.org/10.1017/9781108685047.021
Autor:
Katy Evans, B. Ronald Frost
Publikováno v:
Journal of Petrology. 62
Previous studies have concluded that dehydration of serpentinites in subduction zones produces oxidizing fluids that are the cause of oxidized arc magmas. Here, observations of natural samples and settings are combined with thermodynamic models to ex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55ac934d5856dfe7e8a8f148a2f9709b
https://doi.org/10.1093/petrology/egab016
https://doi.org/10.1093/petrology/egab016
Autor:
Carol D. Frost, B. Ronald Frost
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2f23f9e171b562b04df392a300bd1484
https://doi.org/10.1130/abs/2020am-355273
https://doi.org/10.1130/abs/2020am-355273
Autor:
Carol D. Frost, B. Ronald Frost, David W. Mogk, Darrell J. Henry, Paul A. Mueller, Not Provided, Susan M. Swapp, Fabio Da Prat
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fcbc5fd213a1ab088d71dd0364941d5b
https://doi.org/10.1130/abs/2020am-354771
https://doi.org/10.1130/abs/2020am-354771
Publikováno v:
Geosphere. 14:1031-1050
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6715c0b80cb3f99c456be061ce1072ea
https://doi.org/10.1130/ges01607.1
https://doi.org/10.1130/ges01607.1
Publikováno v:
Geosphere. 2018. Vol. 14, № 3. P. 1008-1030
Although Archean gneisses of the Teton Range crop out over an area of only 50 × 15 km, they provide an important record of the Archean history of the Wyoming Province. The northern and southern parts of the Teton Range record different Archean histo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::163504f8bffdfd42cc16ef6462c70ded
https://doi.org/10.1130/ges01559.1
https://doi.org/10.1130/ges01559.1