Zobrazeno 1 - 10
of 93
pro vyhledávání: '"D L, Hamilton"'
Autor:
S. Singh Dubb, Anand Sardesai, Ghansham Biyani, D. L. Hamilton, Arun James Thirunavukarasu, Ashley Ferro, Cecilia Brassett
Publikováno v:
Clinical anatomy (New York, N.Y.)REFERENCES. 34(7)
Introduction Temporomandibular joint (TMJ) dysfunction is common, with a greater prevalence in females. While magnetic resonance imaging (MRI) is commonly used for clinical investigation, ultrasonography represents a potential alternative in some cli
Autor:
D. L. Hamilton, B. P. Manickam
Publikováno v:
Anaesthesia. 72(12)
Publikováno v:
Mineralogical Magazine. 78:171-202
Experiments in the system NaAlSiO4(Ne)−KAlSiO4(Ks)−SiO2(Qz)−H2O at 100 MPa show that the maximum content of NaAlSi2O6in leucite is ∼4 wt.% and that analcime is close to the stoichiometric composition (NaAlSi2O6.H2O). Analcime forms metastably
Autor:
D. L. Hamilton, D. Skelton
Publikováno v:
Anaesthesia. 72:1158-1159
Autor:
D. L. Hamilton, B. P. Manickam
Publikováno v:
Anaesthesia. 72:915-916
Autor:
D. L. Hamilton, R. M. Jackson
Publikováno v:
European Journal of Anaesthesiology. 15:501-504
Publikováno v:
Contributions to Mineralogy and Petrology. 114:276-287
Three thin, syn-caldera ash flow tuffs of the Suswa volcano, Kenya, contain pumiceous clasts and globules of trachytic glass, and clasts rich in carbonate globules, in a carbonate ash matrix. Petrographic and textural evidence indicates that the carb
Publikováno v:
Journal of Sedimentary Research. 62:520-529
Illite and illite-smectite, with various morphologies, have been formed on quartz grains by precipitation from solution following dissolution of amorphous Al/Si gels at 150-350 degrees C and 0.75-1.0 kbar (75-100 MPa). Initial solutions include deion
Autor:
Anthony F T Brown, D. L. Hamilton
Publikováno v:
Emergency Medicine Journal. 15:111-113
Tick bite anaphylaxis has rarely been reported. It may follow the bite of any of the different tick life cycle forms, is related to the release of salivary juices, and may range from mild itch to severe wheeze or shock. Data obtained suggest that it
Autor:
D. L. Hamilton
Publikováno v:
Petrology
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a1ce2b7605b1bc00e3c0c73da819656
https://doi.org/10.1007/0-387-30845-8_259
https://doi.org/10.1007/0-387-30845-8_259