Geology Reference
In-Depth Information
fluid-mass-transfer. When it is limited by lithological or
tectonic barriers, the gradient value distribution in the sec-
tion forms the opposite correlation: maximization directly
underneath the barrier complex.
7. The existence of the sediment sections in the natural envi-
ronment and the domination of the regional and local
water-exchange by a new type, cross-flow-injection geody-
namic system. This system is dominated by strong present-
day interformational vertical (from the bottom upward)
pulsating ground water cross-flow through the faults, litho-
facies “windows”, elevated fracturing zones in carbonate res-
ervoirs, contacts of diapir intrusions, mud volcano eruption
plugs, etc. emerging during neotectonic activation events.
