1/10/2024 0 Comments Enigma propertiesYou can sort and/or filter them by time of year, review score, and more. language, whether it’s just a rating or contains comments as well, etc.). When you see multiple reviews, the most recent ones will be at the top, subject to a few other factors (e.g. We may stop showing reviews once they’re 36 months old, or if the accommodation has a change of ownership. To make sure reviews are relevant, we may only accept reviews that are submitted within 3 months of checking out. Any violation of our review guidelines.if the writer is claiming to be someone else) Swear words, sexual references, hate speech, discriminatory remarks, threats, or references to violence.However, we won’t display any reviews that include or refer to (among other things): Ideally, we'd publish every review we get, positive and negative. If we find any, we delete them and, if necessary, take action against whoever is responsible.Īnyone who spots something suspicious can always report it to our Customer Service team so that our fraud team can investigate. We have people and automated systems that specialize in detecting fake reviews submitted to our platform. To edit a review you’ve already submitted, contact our Customer Service team. You can review an accommodation that you booked through our platform if you stayed there, or if you got to the property but didn’t actually stay there. Guests submit their subscores and their overall scores independently – there’s no direct link between them. Guests can also give separate subscores in crucial areas, such as location, cleanliness, staff, comfort, facilities, value, and free WiFi. To get the overall score, we add up all the review scores and divide that total by the number of review scores we received. Hence our results apply to gabbros in situ, as well as to the laboratory samples seismic velocities in lower oceanic crust produced at high and intermediate spreading rates are controlled principally by the degree of hydrothermal alteration of the gabbros that compose the lower crust.Start of dialog content How guest reviews workĮach review score is between 1 and 10. The fact that the crack fill consists largely of talc and/or serpentine indicates that these minerals formed by hydrothermal alteration in young, hot (>150☌) lower crust. Adding 11% alteration of olivine to serpentine plus magnetite in the form of crack fill to the Fo73 model yields a nearly exact match between the model and measured P and S wave velocities. Because of its Mg content, olivine that is typical of oceanic gabbros does not influence seismic velocities. Voigt average models show that there is a strong, positive correlation between P wave velocities and Fo90 content but no correlation with Fo73. The Mg content of olivine in these rocks is known to be appreciably less than Fo90, and optical, SEM, and electron microprobe analyses indicate that the “olivine” is actually an aggregate of olivine and 5–15% crack fill consisting of talc and/or serpentine plus magnetite. The objective of this study was to determine whether the effects of low Mg content and/or cracks that typically populate olivine grains can explain why P and S wave velocities in samples of oceanic gabbro do not increase with increasing olivine content.
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |