Place is the correct answer!
Answer:
Hm
You might think I'm crazy
The way I've been craving
If I put it quite plainly
Just give me them babies
So what you doing tonight?
Better say, "Doing you right" (yeah)
Watching movies but
We ain't seeing a thing tonight (yuh)
I don't wanna keep you up (you up)
But show me, can you keep it up? (It up?)
'Cause then I'll have to keep you up
(Bad word) maybe, I'ma keep you up, boy
Explanation:
I hope you can guess this!! :))
The answer is a. //too short
Answer:
Subsidence is so slow that there seems to have been no depression of the upper surface of the lithosphere, so depositional environments are mostly the
same as those in surrounding areas; the succession is just thicker. These
successions are also more complete, however—there are fewer and smaller
diastems—so at times the basin must have remained under water while surrounding areas were emergent. (A diastem is a brief interruption in
sedimentation, with little or no erosion before sedimentation resumes.)
Size, shape: rounded, equidimensional, hundreds of kilometers across
Sediment fill: shallow-water cratonal sediments (carbonates, shales, sandstones),
thicker and more complete than in adjacent areas of the craton but still
relatively thin, hundreds of meters.
Hopefully that helps!