Zobrazeno 1 - 10 of 571 pro vyhledávání: '"D. H. Lindsley"'
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From shifting silt to solid stone: the manufacture of synthetic basalt in ancient mesopotamia
Autor: D. H. Lindsley, E. C. Stone, G. Harbottle, Mark T. Ford, V. Pigott
Publikováno v: Science (New York, N.Y.). 280(5372)
Slabs and fragments of gray-black vesicular “rock,” superficially resembling natural basalt but distinctive in chemistry and mineralogy, were excavated at the second-millennium B.C. Mesopotamian city of Mashkan-shapir, about 80 kilometers south o
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9064a4ea08ab4c30bb04b6101dc8716c
https://pubmed.ncbi.nlm.nih.gov/9641908
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4
Akademický článek
Background optimization of powder electron diffraction for implementation of the e‐PDF technique and study of the local structure of iron oxide nanocrystals.
Autor: Mogili, Naga Vishnu Vardhan1 vishnu.mogili@lnnano.cnpem.br, Verissimo, Nathália Carolina1, Abeykoon, A. M. Milinda2, Bozin, Emil S.3, Bettini, Jefferson1, Leite, Edson Roberto1,4, Souza Junior, João Batista1,5 joao.junior@lnnano.cnpem.br
Publikováno v: Acta Crystallographica. Section A, Foundations & Advances. Sep2023, Vol. 79 Issue 5, p412-426. 15p.
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5
M�ssbauer spectra of synthetic Ca-Fe pyroxenoids and lunar pyroxferroite
Autor: D. H. Lindsley, Eric Dowty
Publikováno v: Contributions to Mineralogy and Petrology. 48:229-232
Resolution of the iron sites in the Mossbauer spectra of Ca-Fe pyroxenoids is only partial, two doublets being apparent in each case, whereas there are up to nine cation sites in each structure. Thus the inner and outer doublets represent, respective
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::1343f16e215c8f00aeee828526a30adb
https://doi.org/10.1007/bf00383358
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7
P-T-oxygen fugacity relations for the system Fe-O-SiO 2
Autor: D. H. Lindsley, R. H. Nafziger, D. H. Speidel
Publikováno v: American Journal of Science. 266:342-360
Intensive-variable phase diagrams are receiving more frequent use by petrologists. Phase relations for the system Fe-O-SiO 2 expressed in P-T-oxygen fugacity (intensive-variable) space provide a necessary building block for more complex but geologica
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b692ec2d9a0b08a556059b6fab8f2639
https://doi.org/10.2475/ajs.266.5.342
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9
Compositions of synthetic augite and hypersthene coexisting at 810°C: Application to pyroxenes from lunar highlands rocks
Autor: H. E. King, A. C. Turnock, D. H. Lindsley
Publikováno v: Geophysical Research Letters. 1:134-136
Hydrothermal experiments on synthetic Ca-Mg.-Fe pyroxenes at 810°C and Pfluid = Ptotal = 15 kbar show that augites coexisting with orthopyroxene range in CaSiO3 content from 43 ± 1 mole percent (Fe/Fe+Mg = 0.18) to 38±1 mole percent (Fe/Fe+Mg = 0.
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::9d8e5ddfdb03eed71bb4c76f4a8709d0
https://doi.org/10.1029/gl001i003p00134
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10
Akademický článek
Oriented α-Fe2O3 and Fe3O4 nanoporous films obtained by topotactic-like pseudomorphic transformation of γ- and δ-FeOOH films.
Autor: Shinagawa, Tsutomu, Kanemoto, Yuya, Ohtaka, Atsushi
Publikováno v: Journal of Materials Chemistry C; 7/21/2024, Vol. 12 Issue 27, p9957-9967, 11p
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