Zobrazeno 1 - 10 of 15 pro vyhledávání: '"Jacob B. Forshaw"'
1
Seeing through metamorphic overprints in Archean granulites: Combined high-resolution thermometry and phase equilibrium modeling of the Lewisian Complex, Scotland
Autor: Phillip Gopon, Jacob B. Forshaw, Jon Wade, David J. Waters, Christine Gopon
Publikováno v: American Mineralogist. 107:1487-1500
The Lewisian Complex in northwest Scotland presents a record of the transition from the Neo-Archean to the Paleoproterozoic. However, this record is complicated by a long and varied history after peak metamorphism that has erased and/or partially res
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::8ff38035320f2905404df552431cbbd7
https://doi.org/10.2138/am-2022-8214ccby
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2
Supplemental Material: Major-element geochemistry of pelites
Autor: David R. Pattison, Jacob B. Forshaw
Detailed methodology, supplemental figures and tables, and references for studies in the database. Whole-rock analyses can be found in the EarthChem repository (https://www.earthchem.org).
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::81eeeb45cca461ce1150dd8ec802d271
https://doi.org/10.1130/geol.s.21200452.v1
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4
Ferrous/ferric (Fe2+/Fe3+) partitioning among silicates in metapelites
Autor: David R. M. Pattison, Jacob B. Forshaw
Publikováno v: Contributions to Mineralogy and Petrology. 176
Fe3+ and XFe3+, defined as Fe3+/(Fe2+ + Fe3+) on a molar basis, are now recognised as key parameters in phase equilibrium modelling. A hindrance is that it is only possible to routinely measure total Fe, and not Fe3+ and Fe2+, in minerals using the e
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::04f1ba6f22b6b73c7ead8c0d2f75e137
https://doi.org/10.1007/s00410-021-01814-4
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7
A comparison of observed and thermodynamically predicted phase equilibria and mineral compositions in mafic granulites
Autor: David R. M. Pattison, David J. Waters, Richard M. Palin, Phillip Gopon, Jacob B. Forshaw
Publikováno v: Journal of Metamorphic Geology. 37:153-179
Recently published activity–composition (a–x) relations for minerals in upper amphibolite- and granulite facies intermediate and basic rocks have expanded our ability to interpret the petrological evolution of these important components of the lo
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bb07a07817ec1849a46ce3056d049f26
https://doi.org/10.1111/jmg.12454
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10
Major-element geochemistry of pelites
Autor: Jacob B. Forshaw, David R.M. Pattison
Publikováno v: Geology
Forshaw, Jacob B.; Pattison, David R.M. (2023). Major-element geochemistry of pelites. Geology, 51(1), pp. 39-43. Geological Society of America 10.1130/G50542.1
Pelites (shales and mudstones) are arguably the most important rock type for interpreting metamorphism. Their significance derives from their widespread occurrence and the range of mineral assemblages they develop at different conditions of pressure
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c0c4f814ce5efcba292dc8f974f0847b
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