Showing 11,281 - 11,300 results of 24,296 for search '(( a step decrease ) OR ( 100 ((((nn decrease) OR (mean decrease))) OR (a decrease)) ))', query time: 0.77s Refine Results
  1. 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. by Armand Paauw (255206)

    Published 2013
    “…<p>A) ROS production in PBMC-derived monocytes pre-incubated with yersiniabactin or iron-saturated yersiniabactin. …”
  2. 11282

    Video_1_Real-Time Speech Emotion Recognition Using a Pre-trained Image Classification Network: Effects of Bandwidth Reduction and Companding.mp4 by Margaret Lech (8890538)

    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. …”
  3. 11283

    Image4_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

    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. …”
  4. 11284

    Image5_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

    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. …”
  5. 11285

    Image9_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

    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. …”
  6. 11286

    Image12_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph... by A. Bénard (13030182)

    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. …”
  7. 11287

    Image2_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

    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. …”
  8. 11288

    Image6_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

    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. …”
  9. 11289

    Image7_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

    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. …”
  10. 11290

    Image11_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph... by A. Bénard (13030182)

    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. …”
  11. 11291

    Image1_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

    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. …”
  12. 11292

    Image8_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

    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. …”
  13. 11293

    Image10_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph... by A. Bénard (13030182)

    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. …”
  14. 11294

    Table1_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

    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. …”
  15. 11295

    Image3_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophi... by A. Bénard (13030182)

    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. …”
  16. 11296

    Image13_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly sideroph... by A. Bénard (13030182)

    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. …”
  17. 11297

    How common ravens (Corvus corax) exploit anthropogenic food sources through time and space in a semi-transformed, alpine environment by Varalika Jain (10659668)

    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. …”
  18. 11298
  19. 11299
  20. 11300