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step decrease » sizes decrease (Expand Search), teer decrease (Expand Search), we decrease (Expand Search)
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11281
ROS production by PBMC-derived monocytes and in the J774A.1 cell line (mouse macrophages) is also reduced by pre-incubation with iron-binding molecules.
Published 2013“…<p>A) ROS production in PBMC-derived monocytes pre-incubated with yersiniabactin or iron-saturated yersiniabactin. …”
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11282
Video_1_Real-Time Speech Emotion Recognition Using a Pre-trained Image Classification Network: Effects of Bandwidth Reduction and Companding.mp4
Published 2020“…<p>This paper examines the effects of reduced speech bandwidth and the μ-low companding procedure used in transmission systems on the accuracy of speech emotion recognition (SER). A step by step description of a real-time speech emotion recognition implementation using a pre-trained image classification network AlexNet is given. …”
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11283
Image4_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11284
Image5_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11285
Image9_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11286
Image12_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11287
Image2_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11288
Image6_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11289
Image7_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11290
Image11_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11291
Image1_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11292
Image8_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11293
Image10_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11294
Table1_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11295
Image3_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11296
Image13_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph...
Published 2022“…Vein sulfides, ranging from Fe-rich MSS (ca. 1,050–1,100°C) to xSS (≤850°C) through Ni-rich MSS, were formed in a sulfide liquid line of descent under oxygen and sulfur fugacity conditions (fO<sub>2</sub> and fS<sub>2</sub>) down to one log unit below the fayalite–magnetite–quartz and close to the Pt-PtS buffers, respectively. …”
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11297
How common ravens (Corvus corax) exploit anthropogenic food sources through time and space in a semi-transformed, alpine environment
Published 2021“…Individuals were also found to extensively exploit resources in spring, both visiting high numbers of AFSs and having a high probability of being present at an AFS, perhaps due to decreased competition (e.g., from breeders) and increases in food availability. …”
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11298
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11299
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11300