Results 151 to 160 of about 17,679 (196)

Simulation dataset of thermal and epithermal neutron self-shielding correction factors for 186W(n,γ)187W reaction rate experiments using tungsten foil targets. [PDF]

Data Brief
Anh TTT, Son PN, Tai CT, Dung TP, Cuong TV, Hieu PBQ, Vu CD.   +6 more
europepmc   +1 more source

Development and evaluation of surface-guided patient position system for boron neutron capture therapy. [PDF]

Sci Rep
Chen J, Xie QL, Ping JJ, Hou TT, Liu YH.
europepmc   +1 more source

Single-shot laser-driven neutron resonance spectroscopy for temperature profiling. [PDF]

Nat Commun
Lan Z, Arikawa Y, Mirfayzi SR, Morace A, Hayakawa T, Sato H, Kamiyama T, Wei T, Tatsumi Y, Koizumi M, Abe Y, Fujioka S, Mima K, Kodama R, Yogo A.   +14 more
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Constraining the impact of chlorine as a neutron absorber in next-gen fast reactor designs. [PDF]

Sci Rep
Hanselman K, Allan IJ, Kuvin SA, Kawano T, Kleedtke N, Lee HY, Paneru SN, Thompson N, Winkelbauer J, Cisneros T, Harper B, Wargon M.   +11 more
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The hydrogen sublattice in hydrated molybdenum trioxides: Insight from multi-energy neutron scattering. [PDF]

Struct Dyn
Drużbicki K, Lalik E, Kosydar R, Gutmann M, da Silva I, Rudić S, Orlandi F, Khalyavin D, Manuel P, Krzystyniak M.   +9 more
europepmc   +1 more source

Development of a multi-layer high-efficiency GEM-based neutron detector for spallation sources. [PDF]

Sci Rep
Cancelli S, Caruggi F, Perelli Cippo E, Putignano O, Celora A, Gorini G, Krzystyniak M, Muraro A, Romanelli G, Pinna RS, Tardocchi M, Croci G.   +11 more
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Epithermal Deposits of Kamchatka, Russia

Geology of Ore Deposits, 2023
The results of studying the epithermal deposits of Kamchatka, one of the most promising gold-mining provinces of the Russian Federation, are generalized. The deposits are divided into acid–sulfate (Ac-Sul) and adularia–sericite (Ad-Ser) types (Heald et al., 1987).
N. S. Bortnikov, N. D. Tolstykh
openaire   +1 more source

Epithermal positron dynamics

Applied Surface Science, 1997
Energetic positrons implanted into a solid rapidly lose energy, down to the order of an electron volt, through plasmon and single electron scattering. However, the later stages of thermalisation are slower, involving predominantly acoustic phonon scattering, with no discrete boundary between the epithermal and thermal equilibrium states.
D.T. Britton, M. Härting
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Volcanism and epithermal deposits

Journal of Volcanology and Seismology, 2015
Epithermal mineralization is an important metallogenic criterion for volcanogenic belts of varying ages. We show that epithermal high-sulfidation deposits are shallow formations in volcanogenic belts, with low-sulfidation deposits being formed at the subvolcanic level and the intermediate between the two types being the deepest deposits.
A. A. Sidorov, A. V. Volkov, N. E. Savva
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Epithermal gold deposits

1999
Abstract Epithermal ore deposits form in the shallow portions of hydrothermal systems, from the surface to less than about 1-km depth. The hydrothermal activity is associated with contemporaneous volcanism and related magma intrusions, and the ore is hosted typically by volcanic rocks.
Jeffrey W. Hedenquist, Antonio Arribas
openaire   +1 more source