טוען...
Constraints on the anisotropic contributions to velocity discontinuities at ∼60 km depth beneath the Pacific
Strong, sharp, negative seismic discontinuities, velocity decreases with depth, are observed beneath the Pacific seafloor at ∼60 km depth. It has been suggested that these are caused by an increase in radial anisotropy with depth, which occurs in global surface wave models. Here we test this hypothe...
שמור ב:
| הוצא לאור ב: | Geochem Geophys Geosyst |
|---|---|
| Main Authors: | , |
| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
John Wiley and Sons Inc.
2017
|
| נושאים: | |
| גישה מקוונת: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5652234/ https://ncbi.nlm.nih.gov/pubmed/29097907 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/2017GC006850 |
| תגים: |
הוספת תג
אין תגיות, היה/י הראשונ/ה לתייג את הרשומה!
|