BarnRat said:
Did the meteor or comet that struck Earth at the end of the Cretaceous punch a whole in the crust down to the mantle? If so, why isn't that part of the crust weak and showing signs of volcanism? Even if the crust wasn't punctured down to the mantle, wouldn't it still be a weak spot and show volcanic signs -- sort of like "hot spots".
Whisper Gallery effect.
I don't claim to know whether the shock wave from "antipodes" theory is correct or not. Some scientists claim that the Deccan Trappes started a million years before the KT impact. However, I am not sure this "fact" will prove robust. However, I can explain the reasoning that goes into the antipodes effect, right or wrong.
The "antipodes theory" claims that the basaltic flow of the Deccan Trappes started on the side opposite the impact because of the whisper gallery effect. The shock waves spread out from the point of impact. However, the shock waves were refocused on the far end of the Earth by the whispering gallery process. The Earth acted like a reflective lens. The basaltic flow was caused by cavitation on the “free” end of the earth, somewhat like the free end of a plate after impact by a projectile.
Here is a link to an article stating the hypothesis.
http://www.dinodatabase.com/dinothry.asp
The shock waves, rippling through the Earth, would take about 80 minutes to travel to the antipode, creating a pipeline of destruction from the depths of the Earth to the surface. It is theorized that a huge eruption, in what is now India, created the great lava fields known as the Deccan Traps about 65 million years ago. However, the antipode to the Deccan Traps is not in the vicinity of the great Chicxulub crater, but rather it is located in what is now the eastern Pacific Ocean where the seabed bears evidence of a major impact. Perhaps, as some experts suggest, two or more meteors struck the Earth simultaneously.
The whispering gallery wave are described here.
http://en.wikipedia.org/wiki/Whispering_gallery_wave
“Whispering-gallery waves, or whispering-gallery modes, are a type of wave that can travel around a concave surface. Originally discovered for sound waves in the whispering gallery of St Paul’s Cathedral, they can exist for light and for other waves, with important applications in nondestructive testing, lasing, cooling and sensing, as well as in astronomy.”
Notice that in ordinary spallation, without a whispering gallery, the major damage occurs opposite the impact site. The multiple fragments are released on the “free end” of the plate. The impacting projectile blocks fragments from flying off at the point of impact. Internal cavitation due to stresses occurs on the free end, not the impacted end.
Here is a link to plate spallation.
http://en.wikipedia.org/wiki/Spallation
“Spallation can occur when a tensile stress wave propagates through a material and can be observed in flat plate impact tests. It is caused by an internal cavitation due to stresses, which are generated by the interaction of stress waves, exceeding the local tensile strength of materials. A fragment or multiple fragments will be created on the free end of the plate. This fragment known as "spall" acts as a secondary projectile with velocities that can be as high as one third of the stress wave speed on the material. This type of failure is typically an effect of high explosive squash head (HESH) charges.”