Gs. Soule et Da. Spratt, EN ECHELON GEOMETRY AND 2-DIMENSIONAL MODEL OF THE TRIANGLE ZONE, GREASE CREEK SYNCLINE AREA, ALBERTA, Bulletin of Canadian petroleum geology, 44(2), 1996, pp. 244-257
Citations number
22
Categorie Soggetti
Energy & Fuels","Geosciences, Interdisciplinary","Engineering, Petroleum
The triangle zone structure examined in this study is a deformed wedge
inserted along a delaminated horizon in the basal Upper Brazeau Forma
tion (Upper Cretaceous elastic unit). The surface expression of the tr
iangle zone is an antiform, with an east-dipping thrust cutting throug
h the core of the antiform. Surface antiforms delineate three en echel
on structures in the Grease Creek area, with a strike length of approx
imately 20 km. A comparison of three balanced cross-sections suggests
the en echelon surface geometry reflects the changing position of the
lower bounding detachment of the intercutaneous wedge. From south to n
orth the structures consistently step eastward. A ''relict'' triangle
zone is interpreted beneath the west flank of the Grease Creek Synclin
e based on interpreted seismic data. The surface culmination of the Wi
ldcat Hills triangle zone, located at the deformation front south of t
he study area, can be traced to the position of this relict triangle z
one, demonstrating that there are two separate en echelon intercutaneo
us wedges. An important implication of the en echelon geometry is that
it produces closure of the structural traps along strike because indi
vidual structures terminate along strike. A composite two-dimensional
model of the triangle zone is presented from the published models and
the Grease Creek study. Important features of this model include a ram
p and flat geometry of the upper detachment and upper and lower detach
ments of the intercutaneous wedge that do not merge. Instead, the toe
of the wedge is a zone between the upper and lower detachments rather
than a distinct tip line. The internal geometry of the triangle zone s
tructure is hinterland-dipping in the study area.