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WASHOUT CREEK 3D Arcis Seismic Solutions is pleased to announce Washout Creek 3D 3C survey located in Township 46, Ranges 6 to 7 W5 and is currently available for immediate subscription. This survey is designed to evaluate multiple zones from the Cretaceous to Devonian, including producing formations such as Cardium, Belly River, Glauconitic, Rock Creek and Duvernay. In addition to this survey’s optimal acquisition parameters, Arcis provides proprietary tools that will enhance imaging and azimuthal fold distribution for even greater assistance with the placement of horizontal wells upon both deep and shallow targets. A TGS COMPANY COMMENCEMENT OF FIELD OPERATIONS IS ANTICIPATED FOR JANUARY 2014 SALES INQUIRIES 2100, 250 - 5 TH Street SW Calgary, Alberta, Canada T2P 0R4 403.781.1700 or 888.269.6840 [email protected] www.arcis.com Printed in Canada A TGS COMPANY BUSINESS DEVELOPMENT Jonathan Banyard Manager, Data Library & Project Development 403.781.1445 | [email protected] Ross Turner Onshore Sales Manager 403.355.1730 | [email protected] Thane McKay Director Imaging & Offshore Multi-client Sales 403.781.5868 | [email protected] Steve Whidden Project Development & Sales Manager, Canada & US Arctic Region 403.781.6232 | [email protected] Mike Kary Senior Manager, Data Management Sales 403.781.1723 | [email protected] Kim Nott Data Management Administrator 403.781.5861 | [email protected] Darla Henderson Business Development 403.781.1442 | [email protected] IMAGING Thane McKay Director Imaging & Offshore Multi-client Sales 403.781.5868 | [email protected] Graziella Kirtland Grech Director, Processing & Reservoir 403.781.1718 | [email protected] Wendy Ohlhauser Geophysical Advisor 403.781.5872 | [email protected] Florence Janzen Imaging Sales Specialist 403.781.1700 | [email protected] WELL DATA Naomi Storey Sales Representative 403.781.1427 | [email protected] GEOSCIENCE James Keay Principal Geoscientist 403.781.1433 | [email protected] Mohammad Hossein Nemati Geoscientist 403.781.1443 | [email protected] Mike Cardell Senior Sales Representative 403.781.1426 | [email protected] Craig Melton Business Developer, Data Library 403.781.6235 | [email protected] Naomi Storey Sales Representative 403.781.1427 | [email protected]

TGS Arcis- Washout Creek 3D Marketing Material

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Page 1: TGS Arcis- Washout Creek 3D Marketing Material

WASHOUTCREEK 3D

Arcis Seismic Solutions is pleased to announce Washout Creek 3D 3C survey located in

Township 46, Ranges 6 to 7 W5 and is currently available for immediate subscription.

This survey is designed to evaluate multiple zones from the Cretaceous to Devonian,

including producing formations such as Cardium, Belly River, Glauconitic, Rock Creek and

Duvernay.

In addition to this survey’s optimal acquisition parameters, Arcis provides proprietary tools

that will enhance imaging and azimuthal fold distribution for even greater assistance with the

placement of horizontal wells upon both deep and shallow targets.

A TGS COMPANY

COMMENCEMENT OF FIELD OPERATIONS IS ANTICIPATED FOR JANUARY 2014

SALES INQUIRIES

2100, 250 - 5TH Street SW Calgary, Alberta, Canada T2P 0R4 403.781.1700 or 888.269.6840 [email protected] www.arcis.comPrinted in Canada

A TGS COMPANY

BUSINESS DEVELOPMENT

Jonathan Banyard Manager, Data Library & Project Development 403.781.1445 | [email protected]

Ross Turner Onshore Sales Manager403.355.1730 | [email protected]

Thane McKay Director Imaging & Offshore Multi-client Sales 403.781.5868 | [email protected]

Steve Whidden Project Development & Sales Manager, Canada & US Arctic Region 403.781.6232 | [email protected]

Mike Kary Senior Manager, Data Management Sales 403.781.1723 | [email protected]

Kim Nott Data Management Administrator 403.781.5861 | [email protected]

Darla Henderson Business Development 403.781.1442 | [email protected]

IMAGING

Thane McKay Director Imaging & Offshore Multi-client Sales 403.781.5868 | [email protected]

Graziella Kirtland Grech Director, Processing & Reservoir 403.781.1718 | [email protected]

Wendy Ohlhauser Geophysical Advisor 403.781.5872 | [email protected]

Florence Janzen Imaging Sales Specialist 403.781.1700 | [email protected]

WELL DATA

Naomi Storey Sales Representative 403.781.1427 | [email protected]

GEOSCIENCE

James Keay Principal Geoscientist 403.781.1433 | [email protected]

Mohammad Hossein NematiGeoscientist 403.781.1443 | [email protected]

Mike Cardell Senior Sales Representative 403.781.1426 | [email protected]

Craig Melton Business Developer, Data Library 403.781.6235 | [email protected]

Naomi Storey Sales Representative 403.781.1427 | [email protected]

Page 2: TGS Arcis- Washout Creek 3D Marketing Material

www.arcis.com Washout Creek 3D

PAGE ONE

Washout Creek 3D Seismic Survey - Approximately 137 km2

FIELD PARAMETERS AND EQUIPMENT SPECIFICATION

Source Line Spacing 280m

Source Interval 40m

Source Dynamite

Source Array 1 x 1kg @ 9m

Receiver Line Spacing 240m

Receiver Interval 40m

Bin Size 20m x 20m

Sample Rate 1ms

Record Length 5 sec

Patch Size 18 x 126

CONFIDENTIAL - NOT FOR DISTRIBUTION WITHOUT CONSENT FROM ARCIS

Cardium

Figure from Geological Atlas of WCSB Data example from Ille Lake 3D

Approximate location of Washout Creek 3D survey with respect to Devonian stratigraphy

Paleozoic

Beaverhill Lake

While it’s obviously challenging to adequately characterize the very thin Cardium formation

with surface seismic, we have had favourable feedback related to our work in the Bakken,

which might bear reasonable analogy to the Cardium play. In that case, the Bakken itself was

deemed to be too thin to admit fracture characterization, but by analyzing the anisotropy in

the thicker overburden, we were able to make certain important inferences about the Bakken

proper. With our high-effort, 3D/3C acquisition parameters, we are seeking favourable spatial

sampling for the wide azimuth coverage which is appropriate for applying various azimuthally

dependent fracture characterization techniques.

In particular, Shear-wave splitting fracture estimates from the 3C processing, as well as the

AVAZ/VVAZ/Curvature fracture estimates from the PP Processing, could give insight into the

fracture regime of the overburden. Further information about the overburden may be gleaned

from the analysis of the VP/VS ratio that comes out of the 3C processing (high values of VP/

VS tend to indicate more local anomalies where the lithology is less competent). We could

conceivably validate these various attributes against production data from nearby wells.

We intend to undertake, as a value added product, the additional processing of the 3C data/

AVAZ/VVAZ/curvature and we will seek production statistics to correlate.