1. A
A’
Play
models
in
Quadrant
16
and
17
in
Norwegian
North
Sea
Channel
feature
in
Lower
Cretaceous/
Upper
Jurassic
Channel
feature
in
Lower
Cretaceous/
Upper
Jurassic
Pinch
out
of
sequence
in
Lower
Cretaceous/
Upper
Jurassic
This
presentaEon
is
made
to
give
some
few
examples
of
tested
and
untested
play
models
in
the
North
Sea.
No
accurate
locaEon
is
given
in
both
straEgraphic
nor
XY
coordinates.
Valioso
Ltd
and
its
authors
is
not
to
be
held
responsible
for
any
inaccuracies
and
errors
in
material
presented
herein,
and
therefore
not
responsible
for
any
acEons
by
any
party
based
on
these
ideas
presented
in
this
presentaEon.

2. PLAYS
I
and
II
A
channel/
lobe
system
with
a
NW
province
area
is
idenEfied
within
these
Blocks.
Several
generaEons
of
these
channels
overlap
each
other,
and
a
complex
distribuEon
of
potenEal
reservoir
units
can
be
idenEfied.
These
features
can
also
act
as
fluid
carriers/
migraEon
path
ways
for
other
play
models
in
area.
III
StraEgraphic
trap
with
pinchout
and/or
fault
dependent
component
IV
Half
graben
features
with
aprone
look
a
like
features
combined
with
potenEal
smaller
highs
in
conjuncEon
with
these.
V
and
VI
At
16/8-­‐1
well
locaEon
the
acousEc
impedance
is
relaEve
high,
but
in
area
just
east
of
locaEon
much
lower
acousEc
impedance
can
be
idenEfied.
PotenEal
new
plays
can
be
idenEfied
east
of
well
locaEon
in
new
structure
which
is
untested.
AcousEc
impedanse
indicate
realEve
thick
high
porosity
zone
at
this
structure
loacEon.
VII
Low
relief
structure
combined
with
a
low
impedance
signature
interval
either
flanking
the
high
or
even
at
the
crest
of
high.
VIII
StraEgraphic
Pinch
out
trap
combined
with
a
low
impedance
interval
VIIII
Low
relief
structure
combined
with
a
low
impedance
interval
with
potenEal
straEgraphic
trap
defined
by
pinch
out
sequence
in
the
high.
Seismic
line
A-­‐A’
through
well
16/8-­‐1
illustrates
several
play
models
which
could
be
pursued
in
this
region
of
the
North
Sea.
The
well
was
located
to
test
a
thrust-­‐faulted
structure
in
a
NE-­‐SW
trending
sub-­‐basin
to
the
southeast
of
the
Utsira
High.
The
primary
objecEve
was
the
basal
Late
Jurassic
sand.
This
sand
was
esEmated
to
have
an
approximate
gross
thickness
of
71
metres.
The
well
was
drilled
in
1978
and
found
to
be
dry.

3. 16/8-­‐1
Play
I
–
StraEgraphic
trap
within
channel
Play
II
–
StraEgraphic
trap
pinch
out
Play
III
–
StraEgraphic
trap
pinch
out/
fault
Play
IV
–
StraEgraphic
trap/fault
Smaller
scale
of
line
above
Another
example
of
Play
I

4. 16/8-­‐1
Play
V
–
Fault
dependant
High
–
low
impedance
Play
VI
–
Fault
dependant
High
–
low
impedance
Play
VII
–
Low
relief
structure–
low
impedance
Play
VIII
–
Pinchout–
low
impedance
Play
VIIII
–
Low
relief
structure–
low
impedance

5. For
further
details
you
can
contact
Valioso
Ltd
and
its
author
for
further
discussions
and
consultaEons.
Contact
details:
www.valioso.rocks
SEg-­‐Arne
Kristoffersen
Director
Valioso
Ltd
Email:
Sak@ec-­‐ba.com
Skype:
sak-­‐pathfinder
Linkedin:
hbp://se.linkedin.com/in/sEgarne/
Facebook:
hbp://www.facebook.com/ukranova