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Showing 11,021 - 11,040 results of 24,510 for search '(( e point decrease ) OR ( 100 ((ng decrease) OR (((nn decrease) OR (a decrease)))) ))', query time: 0.83s Refine Results
  1. 11021
    Validation and predictive accuracy of the cerebrovascular model,

    Validation and predictive accuracy of the cerebrovascular model, by Hadi Esfandi (21387211)

    Published 2025
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  2. 11022
    Pathogen load in control and rough box migratory colonies.

    Pathogen load in control and rough box migratory colonies. by Maggie Shanahan (17879479)

    Published 2024
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  3. 11023
    Image4_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  4. 11024
    Image5_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  5. 11025
    Image9_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  6. 11026
    Image12_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  7. 11027
    Image2_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  8. 11028
    Image6_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  9. 11029
    Image7_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  10. 11030
    Image11_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  11. 11031
    Image1_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  12. 11032
    Image8_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  13. 11033
    Image10_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  14. 11034
    Table1_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.XLSX

    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. …”
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  15. 11035
    Image3_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  16. 11036
    Image13_Spinel harzburgite–derived silicate melts forming sulfide-bearing orthopyroxenite in the lithosphere. Part 2: Sulfide compositions and their chalcophile and highly siderophile trace element signatures.JPEG

    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. …”
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  17. 11037
    Altered dynamics of glucose, insulin and functional beta-cell mass level for patient A after taking the Roux-en-Y gastric bypass surgery.

    Altered dynamics of glucose, insulin and functional beta-cell mass level for patient A after taking the Roux-en-Y gastric bypass surgery. by Boya Yang (14684850)

    Published 2023
    “…<p>The patient is assumed to take the surgery on day 9300 and the obesity-related factor <i>X</i> is postulated to decrease exponentially to zero in approximately a week. …”
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  18. 11038
    Risk ratio of ischemic stroke (A) and intracerebral hemorrhage (B) with atmospheric pressure of the onset day and its daily changes for the last 7 days.

    Risk ratio of ischemic stroke (A) and intracerebral hemorrhage (B) with atmospheric pressure of the onset day and its daily changes for the last 7 days. by Tomoya Mukai (2311078)

    Published 2017
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  19. 11039
    Table 1_Epidemic characteristics and effectiveness of vaccine intervention on rotavirus infection: a real-world observational study in Zhejiang Province, China.docx

    Table 1_Epidemic characteristics and effectiveness of vaccine intervention on rotavirus infection: a real-world observational study in Zhejiang Province, China.docx by Ziping Miao (503264)

    Published 2025
    “…The annual ASRIR of all ages showed a significant upward trend before 2017 (average percentage change [APC] = 21.64%) and then decreased significantly (APC = −23.02%). …”
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  20. 11040
    Image_2_Prospective Study of a Multimodal Convulsive Seizure Detection Wearable System on Pediatric and Adult Patients in the Epilepsy Monitoring Unit.TIF

    Image_2_Prospective Study of a Multimodal Convulsive Seizure Detection Wearable System on Pediatric and Adult Patients in the Epilepsy Monitoring Unit.TIF by Francesco Onorati (288892)

    Published 2021
    “…Thirty-six patients (18 pediatric) experienced a total of 66 CS (35 pediatric). The Sensitivity (corrected for clustered data) was 0.92, with a 95% confidence interval (CI) of [0.85-1.00] for the pediatric population, not significantly different (p > 0.05) from the adult population's Sensitivity (0.94, CI: [0.89–1.00]). …”
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