Zobrazeno 1 - 10
of 20
pro vyhledávání: '"D. H. Lindsley"'
Autor:
S. E. Kesson, D. H. Lindsley
Publikováno v:
1977, Reviews of Lunar Sciences ISBN: 9781118782118
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b0e4880f7168e6d164acd36d45d500c
https://doi.org/10.1002/9781118782118.ch13
https://doi.org/10.1002/9781118782118.ch13
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
https://pubmed.ncbi.nlm.nih.gov/9641908
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
https://doi.org/10.1007/bf00383358
Autor:
S. A. Dixon, D. H. Lindsley
Publikováno v:
American Journal of Science. 276:1285-1301
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f47c6ae7e3935344bea5b138c1e78a4
https://doi.org/10.2475/ajs.276.10.1285
https://doi.org/10.2475/ajs.276.10.1285
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
https://doi.org/10.2475/ajs.266.5.342
Autor:
D. H. Lindsley
Publikováno v:
TMPM Tschermaks Mineralogische und Petrographische Mitteilungen. 35:283-285
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5548648cfdc52850ef259ae81b5c0c2d
https://doi.org/10.1007/bf01191991
https://doi.org/10.1007/bf01191991
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
https://doi.org/10.1029/gl001i003p00134
Publikováno v:
Advances in Physical Geochemistry ISBN: 9781461258735
Phase equilibria in the system Mg2Si2O6-CaMgSi2O6 have been investigated quite thoroughly (see reviews by Lindsley and Dixon, 1976; and Holland et al., 1979). The Di-En join is well recognized as a high-temperature topologic paradigm for much of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e766bd4231370bcb5e087112e6fb7fc3
https://doi.org/10.1007/978-1-4612-5871-1_8
https://doi.org/10.1007/978-1-4612-5871-1_8
Publikováno v:
Science (New York, N.Y.). 144(3614)
The FeSiO(3) (ferrosilite) end member of the pyroxene series is not known as a pure mineral in nature and cannot be synthesized at atmospheric pressure. It is readily synthesized, however, at pressures from 18 to 45 kb and temperatures from 1150 degr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6e2a2eb584e715e5022c89e19cfd9bc3
https://pubmed.ncbi.nlm.nih.gov/17729800
https://pubmed.ncbi.nlm.nih.gov/17729800