Trace element abundances of high-MgO glasses from Kilauea, Mauna Loa and Haleakala volcanoes, Hawaii

T. P. Wagner; D. A. Clague; E. H. Hauri; T. L. Grove

doi:10.1007/s004100050375

Trace element abundances of high-MgO glasses from Kilauea, Mauna Loa and Haleakala volcanoes, Hawaii

Contributions to Mineralogy and Petrology ◽

10.1007/s004100050375 ◽

1998 ◽

Vol 131 (1) ◽

pp. 13-21 ◽

Cited By ~ 9

Author(s):

T. P. Wagner ◽

D. A. Clague ◽

E. H. Hauri ◽

T. L. Grove

Keyword(s):

Trace Element ◽

Element Abundances ◽

Mauna Loa

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Maps showing interpretation, using R-mode factor analysis, of trace-element abundances in stream-sediment samples, Delta 1 degree by 2 degrees Quadrangle, Utah

10.3133/mf2081f ◽

1994 ◽

Keyword(s):

Factor Analysis ◽

Trace Element ◽

Stream Sediment ◽

Sediment Samples ◽

Element Abundances

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Quantitative analysis of trace element abundances in glasses and minerals: a comparison of laser ablation inductively coupled plasma mass spectrometry, solution inductively coupled plasma mass spectrometry, proton microprobe and electron microprobe data

Journal of Analytical Atomic Spectrometry ◽

10.1039/a707972i ◽

1998 ◽

Vol 13 (5) ◽

pp. 477-482 ◽

Cited By ~ 162

Author(s):

Marc D. Norman ◽

William L. Griffin ◽

Norman J. Pearson ◽

Michael O. Garcia ◽

Suzanne Y. O’reilly

Keyword(s):

Mass Spectrometry ◽

Quantitative Analysis ◽

Laser Ablation ◽

Trace Element ◽

Electron Microprobe ◽

Inductively Coupled Plasma ◽

Proton Microprobe ◽

Element Abundances ◽

Inductively Coupled ◽

Plasma Mass Spectrometry

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Rb, Sr and strontium isotopic composition, K/Ar age and large ion lithophile trace element abundances in rocks and glasses from the Wanapitei Lake impact structure

Geochimica et Cosmochimica Acta ◽

10.1016/0016-7037(76)90193-9 ◽

1976 ◽

Vol 40 (1) ◽

pp. 51-57 ◽

Cited By ~ 19

Author(s):

Stephen R. Winzer ◽

R.K.L. Lum ◽

Shuford Schuhmann

Keyword(s):

Isotopic Composition ◽

Trace Element ◽

Impact Structure ◽

Element Abundances

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Trace element abundances of Mauna Kea basalt from phase 2 of the Hawaii Scientific Drilling Project: Petrogenetic implications of correlations with major element content and isotopic ratios

Geochemistry Geophysics Geosystems ◽

10.1029/2002gc000322 ◽

2003 ◽

Vol 4 (6) ◽

pp. n/a-n/a ◽

Cited By ~ 58

Author(s):

S. Huang ◽

F. A. Frey

Keyword(s):

Trace Element ◽

Major Element ◽

Element Content ◽

Isotopic Ratios ◽

Phase 2 ◽

Scientific Drilling ◽

Element Abundances ◽

Drilling Project

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Geochemical evidences of sedimentary-exhalative origin of the shale-hosted PGE–Ag–Au–Zn–Cu occurrences of the Prades Mountains (Catalonia, Spain): trace-element abundances and Sm–Nd isotopes

Journal of Geochemical Exploration ◽

10.1016/j.gexplo.2004.01.002 ◽

2004 ◽

Vol 82 (1-3) ◽

pp. 17-33 ◽

Cited By ~ 22

Author(s):

Carles Canet ◽

Pura Alfonso ◽

Joan Carles Melgarejo ◽

Boris V Belyatsky

Keyword(s):

Trace Element ◽

Nd Isotopes ◽

Element Abundances

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Episodic trace element and isotopic variations in historical Mauna Loa Lavas: Implications for magma and plume dynamics

Mauna Loa Revealed: Structure, Composition, History, and Hazards - Geophysical Monograph Series ◽

10.1029/gm092p0263 ◽

1995 ◽

pp. 263-288 ◽

Cited By ~ 38

Author(s):

J. M. Rhodes ◽

S. R. Hart

Keyword(s):

Trace Element ◽

Mauna Loa ◽

Plume Dynamics ◽

Isotopic Variations ◽

Episodic Trace

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A new locality for primary xenolith-bearing nephelinites in northwestern British Columbia

Canadian Journal of Earth Sciences ◽

10.1139/e85-164 ◽

1985 ◽

Vol 22 (10) ◽

pp. 1556-1559 ◽

Cited By ~ 4

Author(s):

Michael D. Higgins ◽

John M. Allen

Keyword(s):

British Columbia ◽

Trace Element ◽

Volcanic Belt ◽

Primary Magma ◽

Similar Composition ◽

Element Abundances ◽

Late Tertiary

High Ni abundances (420–500 ppm) and Mg* values (100 × Mg/(Mg + Fe2+) = 69–71) and the presence of mantle-derived xenoliths indicate that a subvolcanic nephelinite intrusion in northwestern British Columbia represents an unmodified primary magma. A separate, closely associated nephelinite intrusion shows evidence of minor olivine fractionation from a similar composition. Only three other occurrences of primary nephelinite have been described. This new occurrence suggests that these magmas may not be so rare as previously supposed. The trace-element abundances closely resemble those of primary nephelinites of similar La content from Freemans Cove, Canada. Such compositions are usually taken as evidence of intraplate rifting and doming. Therefore, these rocks are further evidence of late Tertiary or Quaternary rifting in the Stikine volcanic belt.

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26Al, 244Pu, 50Ti, REE, and trace element abundances in hibonite grains from CM and CV meteorites

Geochimica et Cosmochimica Acta ◽

10.1016/0016-7037(87)90245-6 ◽

1987 ◽

Vol 51 (2) ◽

pp. 329-350 ◽

Cited By ~ 144

Author(s):

A.J. Fahey ◽

J.N. Goswami ◽

K.D. McKeegan ◽

E. Zinner

Keyword(s):

Trace Element ◽

Element Abundances

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Evolution of major mineral compositions and trace element abundances during fractional crystallization of a model lunar composition

Geochimica et Cosmochimica Acta ◽

10.1016/0016-7037(76)90005-3 ◽

1976 ◽

Vol 40 (4) ◽

pp. 401-411 ◽

Cited By ~ 24

Author(s):

Michael J. Drake

Keyword(s):

Trace Element ◽

Fractional Crystallization ◽

Element Abundances ◽

Mineral Compositions

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Use of trace element abundances in augite and hornblende to determine the size, connectivity, timing, and evolution of magma batches in a tilted batholith

Geosphere ◽

10.1130/ges00931.1 ◽

2013 ◽

Vol 9 (6) ◽

pp. 1747-1765 ◽

Cited By ~ 10

Author(s):

N. Coint ◽

C. G. Barnes ◽

A. S. Yoshinobu ◽

M. A. Barnes ◽

S. Buck

Keyword(s):

Trace Element ◽

Element Abundances

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