The post you responded to was not my reply to your request for clarification. The approval process messes with the conversation on this board.
One thing: my understanding is that @BrushyCanyon is also a geologist with similar experience to mine. From his writings it is clear to me that @John_Harshman has a decent grounding in geology as well. I would listen to them if I were you.
Glenn Morton - let me quite his words from the TO article:
“They are saying that there is no place on earth where all twelve of the periods are found. Given that the precambrian is always found if one drills deep enough we merely need to find places with the 11 phanerozoic periods. What we will see below is that such situations do occur.”
What he is saying here is that there are places where every period of the geological time scale is represented by actual rocks. What he is emphatically NOT saying is that at these locations there has been unbroken sedimentation since the Precambrian. In fact, he makes that clear:
"There is no place on earth that has sediments from every single day since the origin of the earth. No geologist would require this level of detail from the geological column. But if there are sediments left at a given site once every hundred thousand years or so, then at the scale of the geological column, the entire column would exist.There would still be erosional surfaces contained in that column and that would mean that some days left no sediment at a given location to mark their existence. "
What this means is that a number of places on Earth have been sedimentary basins throughout the Phanerozoic pretty much all of the time. I haven’t checked all of the list but in general I expect these locations to be on stable cratonic interiors - that is, areas away from orogenic belts (past and present mountain ranges) with a largely quiet and undisturbed geological history.
Now I am going to give you a bit of background that will be helpful in understanding what has been going on.
In cratonic areas the Earth’s crust isn’t affected much by the horizontal stresses caused by plate tectonics. Instead, such areas tend to slowly move vertically, down as well as up, in response to deeper processes in the mantle. This is called epeirogenic movement. Such movements may allow the creation of accumulation space for thick piles of sediments (note that the loading caused by the weight of the sediment pile is insufficient by itself to create this accomodation space).
Apart from these vertical crustal movements, which will be different from region to region, there have also been continuous variations in global sea level. The amplitudes of these are in the order of hundreds of meters (note that this is an order of magnitude smaller than what would be required to cover all of the mountains of the Earth with water). Causes for these variations are climatic change (the hotter, the less water is captured as ice) and also the particular state of plate tectonics (for instance active spreading means a lot of extensive underseas volcanic ridges that displace water onto the continental shelves).
The sedimentary record then is the cumulative product of both of these factors. If the net effect is that the area is mostly under water, we can have very continous sedimentation and little erosion. However, there will be times when global sea level fall coincides with local vertical uplift so that the area becomes emerged, and part of the previously deposited column will be eroded away, leaving a gap. To complicate matters, at such times there can still be deposition as well - terrestrial sediments formed in rivers, lakes and deserts. It all depends on the specific local configuration at the time.
Are you with me so far?