I would assume that plate tectonics would be one cause of the rise of the intrusive igneous from the mantel to above the fossil.
One cause. Not the only cause. Certainly, plate boundaries offer more openings for magma to migrate to the surface and we tend to see a lot of volcanic activity around those boundaries; eg, the Pacific "Ring of Fire" -- on Google Earth, check out the Aleutian Islands some time. However, magma may also migrate
in the middle of a plate, two famous examples being the mid-Pacific "hot spot" (currently just east of Hawaii) that has created a long chain of islands and seamounts as the Pacific plate moved over it, and the Yellowstone cauldera (
http://en.wikipedia.org/wiki/Yellowstone_Caldera#Volcanism):
quote:
Yellowstone, like Hawaii, is believed to lie on top of an area called a hotspot where light, hot, molten mantle rock rises towards the surface. While the Yellowstone hotspot is now under the Yellowstone Plateau, it previously helped create the eastern Snake River Plain (to the west of Yellowstone) through a series of huge volcanic eruptions. Although the hotspot's apparent motion is to the east-northeast, the North American Plate is really moving west-southwest over the stationary hotspot deep underneath.
At any rate, the speed of plate tectonic activity or even the very presence of activity has absolutely no bearing on the age of any igneous formations. Rather, it is
when those formations had solidified that determines that. Here is an excellent article on isochron dating,
http://www.talkorigins.org/faqs/isochron-dating.html, which explains that.
Also, here is a link to a textbook,
An Introduction to Physical Science at
http://books.google.com/books?id=1LvMLoaN0HQC&pg=PA710&lp.... That page gives an example of interpreting two igneous intrusions -- it's in Google books, so I'm unable to copy-and-paste. The graphic it refers to is on the next page, so simply scroll down a little bit.