Re: The occurrence of abnormally high gas and oil pressures!


Nashton wrote:
Windy wrote:
NILS BÖRJESSON wrote:
70. The occurrence of abnormally high gas and oil pressures
within relatively permeable rock implies that these fluids
were formed or encased less than 10,000 years ago. If
these hydrocarbons had been trapped OVER 10,000 years ago,
leakage would have dropped the pressure to a level far
below what it is today [a].

The occurrence of abnormally high pressures within Nils's impermeable
head implies that the fluids therein were formed or encased less than
10 years ago. Therefore, the age of Nils cannot be estimated to be
higher than 10 years, unless there is a way to counter the increasing
build-up of pressure. Ranting on Usenet may be one way to relieve it.

-- w.



Oh for crying out loud. Can you ever act like an adult and stop trying
to look "smart" with your ridiculous and impertinent one-liners?


Can you do anything but wait for the frustration level to reach the
point in someone where they make a smart alec response.? I note that
you did not respond to the substantial answers in the previous posts.
It's obvious to everyone here - even you - that Nils will not change
his mind about this, no matter how clearly it has been explained that
all of his "arguments" are long refuted. I predict that he will repeat
this very same argument elsewhere, perhaps here in the near future.

Do you deny this? Do you deny that the previous arguments were correct,
and Nils is full of it, at least on this matter?

Windy understands clearly that there will be no getting thru to Nils.
Nils, alas, is probably not a child, and neither are you. That is just
sad.

Seven out of eight posts have verifiable substance, and you react to
the one expression of frustration (shared by all of us but you).

There's more than a little of the "whistling in the dark" about your
posts, Nicola. Have you convinced yourself yet that you are right?


--
Nicolas

<snip ID theory explained>
<snip founder's admission that ID is not science>

Kermit


.

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