Characterizing major and trace element compositions in fallout melt glass from a near-surface nuclear test

2022 ◽  
Vol 243 ◽  
pp. 106796
Author(s):  
Josh Wimpenny ◽  
Gary R. Eppich ◽  
Naomi Marks ◽  
Frederick Ryerson ◽  
Kim B. Knight
Keyword(s):  
Trace Element ◽  
Nuclear Test ◽  
Near Surface ◽  
Melt Glass

scholarly journals Constraints on fallout melt glass formation from a near-surface nuclear test

2014 ◽  
Vol 302 (1) ◽  
pp. 593-609 ◽  
Author(s):  
Gary R. Eppich ◽  
Kim B. Knight ◽  
Timothy W. Jacomb-Hood ◽  
Gregory D. Spriggs ◽  
Ian D. Hutcheon
Keyword(s):  
Glass Formation ◽  
Nuclear Test ◽  
Near Surface ◽  
Melt Glass

scholarly journals Diffusive mass transport in agglomerated glassy fallout from a near-surface nuclear test

2018 ◽  
Vol 223 ◽  
pp. 377-388 ◽  
Author(s):  
David G. Weisz ◽  
Benjamin Jacobsen ◽  
Naomi E. Marks ◽  
Kim B. Knight ◽  
Brett H. Isselhardt ◽  
...  
Keyword(s):  
Mass Transport ◽  
Nuclear Test ◽  
Near Surface

scholarly journals Deposition of vaporized species onto glassy fallout from a near-surface nuclear test

2017 ◽  
Vol 201 ◽  
pp. 410-426 ◽  
Author(s):  
David G. Weisz ◽  
Benjamin Jacobsen ◽  
Naomi E. Marks ◽  
Kim B. Knight ◽  
Brett H. Isselhardt ◽  
...  
Keyword(s):  
Nuclear Test ◽  
Near Surface

Trace element composition of near-surface silica deposits—A powerful tool for detecting hydrothermal mineral and energy resources

2011 ◽  
Vol 280 (1-2) ◽  
pp. 154-169 ◽  
Author(s):  
I. Tonguç Uysal ◽  
Massimo Gasparon ◽  
Robert Bolhar ◽  
Jian-xin Zhao ◽  
Yue-xing Feng ◽  
...  
Keyword(s):  
Trace Element ◽  
Trace Element Composition ◽  
Element Composition ◽  
Energy Resources ◽  
Near Surface ◽  
Surface Silica ◽  
Hydrothermal Mineral

scholarly journals A synchrotron X-ray spectroscopy study of titanium co-ordination in explosive melt glass derived from the trinity nuclear test

RSC Advances ◽  
2019 ◽  
Vol 9 (23) ◽  
pp. 12921-12927
Author(s):  
D. J. Bailey ◽  
M. C. Stennett ◽  
B. Ravel ◽  
D. E. Crean ◽  
N. C. Hyatt
Keyword(s):  
Absorption Spectroscopy ◽  
Nuclear Test ◽  
Spectroscopy Study ◽  
X Ray ◽  
Melt Glass ◽  
X Ray Absorption ◽  
The Trinity

This work presents the first determination of Ti speciation and co-ordination in trinitite via the use of X-ray absorption spectroscopy.

Trace element and Sr isotopic composition of bottom and near-surface oceanic water in the southern region of the Emperor Ridge

2020 ◽  
Vol 224 ◽  
pp. 103808
Author(s):  
I.A. Vishnevskaya ◽  
T.G. Okuneva ◽  
D.V. Kiseleva ◽  
N.G. Soloshenko ◽  
M.V. Streletskaya ◽  
...  
Keyword(s):  
Isotopic Composition ◽  
Trace Element ◽  
Southern Region ◽  
Oceanic Water ◽  
Near Surface

Picritic magmas and the Rum ultramafic complex, Scotland

2002 ◽  
Vol 139 (4) ◽  
pp. 437-452 ◽  
Author(s):  
B. G. J. UPTON ◽  
A. C. SKOVGAARD ◽  
J. McCLURG ◽  
L. KIRSTEIN ◽  
M. CHEADLE ◽  
...  
Keyword(s):  
Trace Element ◽  
Mantle Source ◽  
Late Stage ◽  
Temporal Change ◽  
Near Surface ◽  
Volcanic Province ◽  
Three Samples ◽  
Depleted Mantle ◽  
Ultramafic Complex ◽  
Iceland Plume

Three small picritic dykes, intruded at a late stage in the evolution of the Rum basic–ultra-basic complex, Inner Hebrides, shed new light on the nature of the magmas responsible for the main complex. The magmas are of transitional (mildly alkalic) type, generated by relatively small-fraction (6–7%) melting of a depleted mantle source. Melting is tentatively deduced to have commenced at ±100 km, straddling the garnet–spinel transition. Of the three samples, one (M9) is remarkable for the preservation of very primitive characteristics, with olivines of Fo93 containing highly aluminous spinels; these appear unique within the British Tertiary Volcanic Province. Sr, Nd and Pb isotopes indicate only minor ([les ]4%) contamination with Precambrian crustal lithologies, reflecting the rapidity of ascent of the magma batches. The Rum picrites have 187Os/188Os ratios and trace element characteristics comparable to those of recent picrites from Iceland, suggesting minimal temporal change of the depleted parts of the Iceland plume over 60 Ma. Movements of the Long Loch Fault may have been instrumental in causing decompression melting of the spreading Iceland plume-head and facilitating ascent of the melts to near-surface levels.

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