Results 101 to 110 of about 26,385 (251)
Plagioclase-alkali feldspar geothermometry revisited
SUMMARY, The plagioclase-alkali-feldspar geothermometer formulated by Stormer 0975) does not take into account the effect of small amounts of calcium in the alkali feldspar.
Marjorie Powell, Roger Powell
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ABSTRACT Previous studies have documented genetic divergence within the last few million years between northern and southern populations of terrestrial plants and animals along the Baja California peninsula, with many studies hypothesising that the divergence is due to an ancient seaway that crossed the central peninsula and created a physical barrier ...
Kevin K. Gardner +8 more
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(Table 6) Representative plagioclase compositions of plagioclase-phyric chilled margins and microdikes of ODP Hole 140 ...
Andrew W McNeill (6973100) +1 more
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ABSTRACT This study investigated the formation mechanism responsible for anomalously high permeability (AHP) observed in the Eocene sandstones at depths from 3824 to 3832 m in the Huizhou Sag, Pearl River Mouth Basin, China, using helium porosity and permeability measurements, thin section, scanning electron microscopy, electron probe X‐ray ...
Changgui Xu +12 more
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(Tabel S5b) Plagioclase-hosted melt inclusions, host plagioclase composition adjacent to inclusion, and thermobarometry of melt inclusion - host mineral ...
Melanie Siegburg (6968786) +7 more
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(Table 1) Modal composition of olivine-plagioclase phyric and plagioclase phyric basalts at DSDP Leg 67 ...
Yuri I Dmitriev (6887309) +1 more
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The thermoluminescence (TL) method is one of the most widely used techniques in various studies, including dosimetric applications, dating of archaeological and geological materials, luminescence spectroscopy of certain insulating or semiconducting ...
Mehmet Yüksel, Emre Ünsal
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Hornblende-plagioclase bearing rocks occur as layers and lenses within metasedimentary rocks of the Esplanade Range, British Columbia (51°31′ N, 117°27′ W).
C. D. S. DeVries, Edward D. Ghent
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Abstract Modeling processes within Earth's and other planetary bodies' mantle requires constraints from phase equilibrium to infer how changes in phase abundance and composition affect physical properties and geochemical processes. When applying such thermodynamic models on a planetary scale, performance becomes especially crucial.
Philip Hartmeier, Pierre Lanari
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