AAPG/GSTT HEDBERG CONFERENCE
“Mobile Shale Basins – Genesis, Evolution and
Hydrocarbon Systems”
Remobilization of Mud Volcano Cones: Shah Deniz, South
Joshua Creviere Turner
BP,
The interpreted geometry of mud volcanos
at depth is often a source of heated debate and concern when exploring for
hydrocarbons in the
On the Shah Deniz
structure, I observe a mud volcano, characterized by a relatively small
syncline, lying disharmonically over the top of the
larger anticline that sets up the field.
It is not significantly perturbed by faulting or subsidence in the mud
volcano’s vicinity. Additionally, the evaporite beds of the upper Surakhany
are usually absent where cones have been remobilized. However, these same evaporites onlap cones that have not been remobilized. Therefore, I believe Shah Deniz’
mud volcanoes were, in general, initially extruded at the surface near the end
of the Surakhany period, but before the deposition of
the evaporite beds initiated; extrusion coincides
with the onset of increased regional shortening. The topographically high cone was then onlapped by evaporites and
subsequently buried by marine sediments.
In the late Pleistocene the cone was remobilized and evacuated, and the
overburden collapsed to form a shallow and local depression. This theory is encouraging for those
developing resources in the Caspian because it reduces risk of reservoir
compartmentalization in the vicinity of a mud volcano and increases the chances
that the reservoir is more extensive and producible beneath mud volcano cones.
AAPG Search and Discovery Article #90057©2006 AAPG/GSTT Hedberg Conference, Port of Spain, Trinidad & Tobago