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#earthquakescience β€” Public Fediverse posts

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  1. Rock Friction Research Reframes Earthquake Mechanics

    Scientists are studying how rock bonds break to understand earthquakes better. This new research affects how we predict and prepare for seismic events.

    #EarthquakeScience, #RockMechanics, #FaultLines, #Seismology, #Geology

    newsletter.tf/rock-friction-re

  2. Rock Friction Research Reframes Earthquake Mechanics

    Scientists are studying how rock bonds break to understand earthquakes better. This new research affects how we predict and prepare for seismic events.

    #EarthquakeScience, #RockMechanics, #FaultLines, #Seismology, #Geology

    newsletter.tf/rock-friction-re

  3. Rock Friction Research Reframes Earthquake Mechanics

    Scientists are studying how rock bonds break to understand earthquakes better. This new research affects how we predict and prepare for seismic events.

    #EarthquakeScience, #RockMechanics, #FaultLines, #Seismology, #Geology

    newsletter.tf/rock-friction-re

  4. Rock Friction Research Reframes Earthquake Mechanics

    Scientists are studying how rock bonds break to understand earthquakes better. This new research affects how we predict and prepare for seismic events.

    #EarthquakeScience, #RockMechanics, #FaultLines, #Seismology, #Geology

    newsletter.tf/rock-friction-re

  5. New research shows that the breaking of bonds between rocks, not just rubbing, is key to how earthquakes start. This is a new way to look at fault lines.

    #EarthquakeScience, #RockMechanics, #FaultLines, #Seismology, #Geology
    newsletter.tf/rock-friction-re

  6. New research shows that the breaking of bonds between rocks, not just rubbing, is key to how earthquakes start. This is a new way to look at fault lines.

    #EarthquakeScience, #RockMechanics, #FaultLines, #Seismology, #Geology
    newsletter.tf/rock-friction-re

  7. New research shows that the breaking of bonds between rocks, not just rubbing, is key to how earthquakes start. This is a new way to look at fault lines.

    #EarthquakeScience, #RockMechanics, #FaultLines, #Seismology, #Geology
    newsletter.tf/rock-friction-re

  8. New research shows that the breaking of bonds between rocks, not just rubbing, is key to how earthquakes start. This is a new way to look at fault lines.

    #EarthquakeScience, #RockMechanics, #FaultLines, #Seismology, #Geology
    newsletter.tf/rock-friction-re

  9. πŸŒ‹πŸŒŠπŸ“‰ Beneath Japan lurks the Kumano Pluton, a mountain of frozen magma bending the crust and steering megaquakes to its flanks. Quakes in ’44 and ’46 proved its pull. Now mapped in 3D, this buried giant may be the key to predicting the next killer tremor. #EarthquakeScience sciencealert.com/a-mountain-si

  10. πŸŒ‹πŸŒŠπŸ“‰ Beneath Japan lurks the Kumano Pluton, a mountain of frozen magma bending the crust and steering megaquakes to its flanks. Quakes in ’44 and ’46 proved its pull. Now mapped in 3D, this buried giant may be the key to predicting the next killer tremor. #EarthquakeScience sciencealert.com/a-mountain-si

  11. A research from 2023 reveals how large-N infrasound arrays and advanced CLEAN beamforming can detect seismic ground shaking remotely via atmospheric sound waves πŸŒπŸ”Š. This method enhances earthquake monitoring and hazard assessment over wide areas. Read more: nature.com/articles/s43247-023 #Seismology #EarthquakeScience #Infrasound

  12. A research from 2023 reveals how large-N infrasound arrays and advanced CLEAN beamforming can detect seismic ground shaking remotely via atmospheric sound waves πŸŒπŸ”Š. This method enhances earthquake monitoring and hazard assessment over wide areas. Read more: nature.com/articles/s43247-023 #Seismology #EarthquakeScience #Infrasound

  13. A research from 2023 reveals how large-N infrasound arrays and advanced CLEAN beamforming can detect seismic ground shaking remotely via atmospheric sound waves πŸŒπŸ”Š. This method enhances earthquake monitoring and hazard assessment over wide areas. Read more: nature.com/articles/s43247-023 #Seismology #EarthquakeScience #Infrasound

  14. A research from 2023 reveals how large-N infrasound arrays and advanced CLEAN beamforming can detect seismic ground shaking remotely via atmospheric sound waves πŸŒπŸ”Š. This method enhances earthquake monitoring and hazard assessment over wide areas. Read more: nature.com/articles/s43247-023

  15. A research from 2023 reveals how large-N infrasound arrays and advanced CLEAN beamforming can detect seismic ground shaking remotely via atmospheric sound waves πŸŒπŸ”Š. This method enhances earthquake monitoring and hazard assessment over wide areas. Read more: nature.com/articles/s43247-023 #Seismology #EarthquakeScience #Infrasound

  16. πŸŒπŸ”Š Earthquakes create infrasonic boomsβ€”low-frequency vibrations the Earth’s surface sends into the air like a giant speaker! These infrasounds can help quickly assess quake damage and distinguish natural quakes from underground explosions. Fascinating science below human hearing! πŸ‘‚πŸŒ #EarthquakeScience #Infrasound #Geophysics livescience.com/24209-earthqua

  17. πŸŒπŸ”Š Earthquakes create infrasonic boomsβ€”low-frequency vibrations the Earth’s surface sends into the air like a giant speaker! These infrasounds can help quickly assess quake damage and distinguish natural quakes from underground explosions. Fascinating science below human hearing! πŸ‘‚πŸŒ #EarthquakeScience #Infrasound #Geophysics livescience.com/24209-earthqua

  18. πŸŒπŸ”Š Earthquakes create infrasonic boomsβ€”low-frequency vibrations the Earth’s surface sends into the air like a giant speaker! These infrasounds can help quickly assess quake damage and distinguish natural quakes from underground explosions. Fascinating science below human hearing! πŸ‘‚πŸŒ #EarthquakeScience #Infrasound #Geophysics livescience.com/24209-earthqua

  19. πŸŒπŸ”Š Earthquakes create infrasonic boomsβ€”low-frequency vibrations the Earth’s surface sends into the air like a giant speaker! These infrasounds can help quickly assess quake damage and distinguish natural quakes from underground explosions. Fascinating science below human hearing! πŸ‘‚πŸŒ livescience.com/24209-earthqua

  20. πŸŒπŸ”Š Earthquakes create infrasonic boomsβ€”low-frequency vibrations the Earth’s surface sends into the air like a giant speaker! These infrasounds can help quickly assess quake damage and distinguish natural quakes from underground explosions. Fascinating science below human hearing! πŸ‘‚πŸŒ #EarthquakeScience #Infrasound #Geophysics livescience.com/24209-earthqua

  21. A study from 2021reveals how infrasound sensors in Japan detect earthquake signals, including unique oceanic coupling via T-phase waves 🌊🌍. Advances in monitoring could enhance early warning systems and seismic research. Dive deeper: pmc.ncbi.nlm.nih.gov/articles/ #EarthquakeScience #Infrasound #Japan #Seismology

  22. A study from 2021reveals how infrasound sensors in Japan detect earthquake signals, including unique oceanic coupling via T-phase waves 🌊🌍. Advances in monitoring could enhance early warning systems and seismic research. Dive deeper: pmc.ncbi.nlm.nih.gov/articles/ #EarthquakeScience #Infrasound #Japan #Seismology

  23. A study from 2021reveals how infrasound sensors in Japan detect earthquake signals, including unique oceanic coupling via T-phase waves 🌊🌍. Advances in monitoring could enhance early warning systems and seismic research. Dive deeper: pmc.ncbi.nlm.nih.gov/articles/ #EarthquakeScience #Infrasound #Japan #Seismology

  24. A study from 2021reveals how infrasound sensors in Japan detect earthquake signals, including unique oceanic coupling via T-phase waves 🌊🌍. Advances in monitoring could enhance early warning systems and seismic research. Dive deeper: pmc.ncbi.nlm.nih.gov/articles/

  25. A study from 2021reveals how infrasound sensors in Japan detect earthquake signals, including unique oceanic coupling via T-phase waves 🌊🌍. Advances in monitoring could enhance early warning systems and seismic research. Dive deeper: pmc.ncbi.nlm.nih.gov/articles/ #EarthquakeScience #Infrasound #Japan #Seismology

  26. Mid-crustal depth earthquakes in Cochabamba-Bolivia?

    Yes, Fernandez et al. provide valuable insights into these earthquakes and show how they are concentrated in the main thrust fault shear zone.

    Read now: doi.org/10.26443/seismica.v4i1

    #Bolivia #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  27. Mid-crustal depth earthquakes in Cochabamba-Bolivia?

    Yes, Fernandez et al. provide valuable insights into these earthquakes and show how they are concentrated in the main thrust fault shear zone.

    Read now: doi.org/10.26443/seismica.v4i1

    #Bolivia #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  28. Mid-crustal depth earthquakes in Cochabamba-Bolivia?

    Yes, Fernandez et al. provide valuable insights into these earthquakes and show how they are concentrated in the main thrust fault shear zone.

    Read now: doi.org/10.26443/seismica.v4i1

    #Bolivia #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  29. Mid-crustal depth earthquakes in Cochabamba-Bolivia?

    Yes, Fernandez et al. provide valuable insights into these earthquakes and show how they are concentrated in the main thrust fault shear zone.

    Read now: doi.org/10.26443/seismica.v4i1

    #Bolivia #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  30. Bolton et al. show that static stresses induced from a nearby ML 4.0 foreshock significantly perturbed the local stress state and could have triggered the 2020 Mentone Mw 4.8 earthquake in West Texas.

    doi.org/10.26443/seismica.v3i2

    #Texas #mentone #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  31. Bolton et al. show that static stresses induced from a nearby ML 4.0 foreshock significantly perturbed the local stress state and could have triggered the 2020 Mentone Mw 4.8 earthquake in West Texas.

    doi.org/10.26443/seismica.v3i2

    #Texas #mentone #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  32. Bolton et al. show that static stresses induced from a nearby ML 4.0 foreshock significantly perturbed the local stress state and could have triggered the 2020 Mentone Mw 4.8 earthquake in West Texas.

    doi.org/10.26443/seismica.v3i2

    #Texas #mentone #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  33. Bolton et al. show that static stresses induced from a nearby ML 4.0 foreshock significantly perturbed the local stress state and could have triggered the 2020 Mentone Mw 4.8 earthquake in West Texas.

    doi.org/10.26443/seismica.v3i2

    #Texas #mentone #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  34. What are reliable earthquake magnitudes?

    Dahm et al.'s method uses synthetic seismogram peak-values to calculate moment magnitudes of microearthquakesβ€”essential for studying shallow, human-induced seismicity:

    doi.org/10.26443/seismica.v3i2

    #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  35. What are reliable earthquake magnitudes?

    Dahm et al.'s method uses synthetic seismogram peak-values to calculate moment magnitudes of microearthquakesβ€”essential for studying shallow, human-induced seismicity:

    doi.org/10.26443/seismica.v3i2

    #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  36. What are reliable earthquake magnitudes?

    Dahm et al.'s method uses synthetic seismogram peak-values to calculate moment magnitudes of microearthquakesβ€”essential for studying shallow, human-induced seismicity:

    doi.org/10.26443/seismica.v3i2

    #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  37. What are reliable earthquake magnitudes?

    Dahm et al.'s method uses synthetic seismogram peak-values to calculate moment magnitudes of microearthquakesβ€”essential for studying shallow, human-induced seismicity:

    doi.org/10.26443/seismica.v3i2

    #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  38. Finite-fault rupture models, without the finite-fault?

    Thurin demonstrates it is possible to simplify the classical representation for large earthquakes using moment tensor interpolation.

    seismica.library.mcgill.ca/art

    #moment-tensor #finitefault #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  39. Finite-fault rupture models, without the finite-fault?

    Thurin demonstrates it is possible to simplify the classical representation for large earthquakes using moment tensor interpolation.

    seismica.library.mcgill.ca/art

    #moment-tensor #finitefault #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  40. Finite-fault rupture models, without the finite-fault?

    Thurin demonstrates it is possible to simplify the classical representation for large earthquakes using moment tensor interpolation.

    seismica.library.mcgill.ca/art

    #moment-tensor #finitefault #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  41. Finite-fault rupture models, without the finite-fault?

    Thurin demonstrates it is possible to simplify the classical representation for large earthquakes using moment tensor interpolation.

    seismica.library.mcgill.ca/art

    #moment-tensor #finitefault #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  42. After more than two years of monitoring the resonance frequency of a rock tower in Utah, Moore et al. show that frequencies drift with daily and annual insolation patterns, which is key for understanding and identifying changes caused by rock damage.

    doi.org/10.26443/seismica.v3i2

    #Utah #rock #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  43. After more than two years of monitoring the resonance frequency of a rock tower in Utah, Moore et al. show that frequencies drift with daily and annual insolation patterns, which is key for understanding and identifying changes caused by rock damage.

    doi.org/10.26443/seismica.v3i2

    #Utah #rock #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  44. After more than two years of monitoring the resonance frequency of a rock tower in Utah, Moore et al. show that frequencies drift with daily and annual insolation patterns, which is key for understanding and identifying changes caused by rock damage.

    doi.org/10.26443/seismica.v3i2

    #Utah #rock #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  45. After more than two years of monitoring the resonance frequency of a rock tower in Utah, Moore et al. show that frequencies drift with daily and annual insolation patterns, which is key for understanding and identifying changes caused by rock damage.

    doi.org/10.26443/seismica.v3i2

    #Utah #rock #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  46. Mita Uthaman et al. examine the northeastern Indian state of Sikkim, which spans approximately 200 km in the Himalayas, and find that it exhibits highly varied site characteristics, indicating significant seismic risk potential.

    doi.org/10.26443/seismica.v3i2

    #Seismicrisk #hazard #himalaya #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  47. Mita Uthaman et al. examine the northeastern Indian state of Sikkim, which spans approximately 200 km in the Himalayas, and find that it exhibits highly varied site characteristics, indicating significant seismic risk potential.

    doi.org/10.26443/seismica.v3i2

    #Seismicrisk #hazard #himalaya #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  48. Mita Uthaman et al. examine the northeastern Indian state of Sikkim, which spans approximately 200 km in the Himalayas, and find that it exhibits highly varied site characteristics, indicating significant seismic risk potential.

    doi.org/10.26443/seismica.v3i2

    #Seismicrisk #hazard #himalaya #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  49. Mita Uthaman et al. examine the northeastern Indian state of Sikkim, which spans approximately 200 km in the Himalayas, and find that it exhibits highly varied site characteristics, indicating significant seismic risk potential.

    doi.org/10.26443/seismica.v3i2

    #Seismicrisk #hazard #himalaya #Seismology #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  50. Sabermahani and Frederiksen developed a new model for quality control in receiver function analysis, designed to identify high-quality signals and ensure that only the most reliable data is preserved for accurate seismic interpretation.

    doi.org/10.26443/seismica.v3i2

    #Seismology #Geophysics #DataScience #Research
    #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  51. Sabermahani and Frederiksen developed a new model for quality control in receiver function analysis, designed to identify high-quality signals and ensure that only the most reliable data is preserved for accurate seismic interpretation.

    doi.org/10.26443/seismica.v3i2

    #Seismology #Geophysics #DataScience #Research
    #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  52. Sabermahani and Frederiksen developed a new model for quality control in receiver function analysis, designed to identify high-quality signals and ensure that only the most reliable data is preserved for accurate seismic interpretation.

    doi.org/10.26443/seismica.v3i2

    #Seismology #Geophysics #DataScience #Research
    #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  53. Sabermahani and Frederiksen developed a new model for quality control in receiver function analysis, designed to identify high-quality signals and ensure that only the most reliable data is preserved for accurate seismic interpretation.

    doi.org/10.26443/seismica.v3i2

    #Seismology #Geophysics #DataScience #Research
    #EarthquakeScience #peerreviewed #DiamondOpenAccess #Earthquake #OpenAccess #OpenScience

  54. Exciting updates at Seismica!
    We've refreshed our journal policies to improve transparency, ethics, and efficiency.
    Check out changes to data requirements, expanded scope, and moreβ€”now easier to find.

    Learn more: seismica.library.mcgill.ca/pol

    #policies #scientificjournal #peerreviewed #openaccess #openscience #Seismology #EarthquakeScience

  55. Exciting updates at Seismica!
    We've refreshed our journal policies to improve transparency, ethics, and efficiency.
    Check out changes to data requirements, expanded scope, and moreβ€”now easier to find.

    Learn more: seismica.library.mcgill.ca/pol

    #policies #scientificjournal #peerreviewed #openaccess #openscience #Seismology #EarthquakeScience

  56. Exciting updates at Seismica!
    We've refreshed our journal policies to improve transparency, ethics, and efficiency.
    Check out changes to data requirements, expanded scope, and moreβ€”now easier to find.

    Learn more: seismica.library.mcgill.ca/pol

    #policies #scientificjournal #peerreviewed #openaccess #openscience #Seismology #EarthquakeScience