TGS-NOPEC Geophysical Company and Subsidiaries v. Commissioner

155 T.C. No. 3
United States Tax Court·Decided August 26, 2020·No. 28140-14·Published

Opinion

155 T.C. No. 3

UNITED STATES TAX COURT

TGS-NOPEC GEOPHYSICAL COMPANY AND SUBSIDIARIES, Petitioner v.

COMMISSIONER OF INTERNAL REVENUE, Respondent

Docket No. 28140-14. Filed August 26, 2020.

R disallowed P’s claimed I.R.C. sec. 199 deduction of $1,946,324 for the 2008 tax year. R determined that P’s gross receipts from the leasing of processed marine seismic data are not considered domestic production gross receipts (DPGR).

Held: P’s processed marine seismic data is not qualifying production property within the meaning of I.R.C. sec. 199(c)(5)

because it is neither tangible personal property nor a sound recording.

Held, further, P’s processing of marine seismic data constitutes engineering services performed in the United States with respect to the construction of real property under I.R.C. sec. 199(c)(4), but its gross receipts from such services are DPGR only to the extent that such construction activities are within the United States.

Held, further, to the extent that P received gross receipts from its parent company for processing services of its parent’s data for the parent’s clients, such revenue does not constitute DPGR.

Val J. Albright, Michelle Y. Ku, and Brent C. Gardner, Jr., for petitioner.

Bettina M. Nadler, Carol B. McClure, and Ashley V. Targac, for respondent.

PARIS, Judge: Respondent determined a deficiency of $858,392 with respect to petitioner’s Federal income tax for 2008. The deficiency is based on respondent’s disallowance of a claimed deduction of $1,946,324 for income attributable to domestic production activities, pursuant to section 199.1 The issue for decision is whether petitioner is entitled to the deduction.

Petitioner bears the burden of proof. See Rule 142(a).2 FINDINGS OF FACT

I. Petitioner’s Background Petitioner consists of TGS-NOPEC Geophysical Co., Inc. (TGS), and its subsidiaries, which together make up an affiliated group of corporations that files

1 Unless otherwise indicated, all section references are to the Internal Revenue Code (Code) in effect for the year in issue, and all Rule references are to the Tax Court Rules of Practice and Procedure.

2 Petitioner has not raised the issue of sec. 7491(a), which shifts the burden of proof to the Commissioner in certain situations. The Court concludes that sec. 7491(a) does not apply here because petitioner has not produced evidence that it has satisfied the preconditions for its application.

a consolidated return for Federal income tax purposes. TGS is a corporation organized and existing under the laws of the State of Delaware. It is a wholly owned subsidiary of TGS-NOPEC Geophysical Co. ASA, a public limited liability company formed under the laws of Norway. Stock in TGS-NOPEC Geophysical Co. ASA is traded on the Oslo Stock Exchange under the symbol “TGS”.

For 2008 petitioner maintained its books and records using the accrual method of accounting and computed its income on the basis of a calendar year. At the time it filed its petition, petitioner’s principal place of business was in Houston, Texas. II. Petitioner’s Business Activities A. Overview Petitioner is engaged in the business of acquiring, processing, and licensing marine seismic data. During 2008 petitioner earned revenue by licensing the processed seismic data to companies in the oil and gas industry. As discussed below, raw seismic data is collected through seismic surveys, during which reflected energy waves are recorded on magnetic tapes. The data on those tapes is then processed to develop an image of subsurface geophysical structures. The processed data is ultimately purchased or licensed by companies in the oil and gas

industry to explore for hydrocarbon deposits and to develop drilling and production equipment.

As of December 31, 2008, petitioner employed 531 individuals in the United States. For 2008 petitioner reported salary and wage payments totaling $27,296,140. Among its employees, petitioner employed a specialized imaging services team (imaging team) of approximately 55 individuals with advanced degrees or extensive experience in mathematics or the physical sciences. The imaging team was responsible for processing the raw seismic data.

Most of the raw data processed in 2008 was acquired from marine seismic surveys that were completed before the year in issue.

B. Marine Seismic Data Acquisition Background The process of marine seismic data acquisition involves the recording and measurement of the travel time of seismic waves from a known energy source at or near the ocean’s surface to various depths in the earth’s subsurface. Generally, to conduct a seismic survey, petitioner would hire a marine vessel equipped with computers, sourcing equipment, and recording equipment.3

3 During 2008 petitioner did not own any seismic vessels and did not own the vessels when the subject raw seismic data was collected. Rather, petitioner would contract for vessels and crews to acquire survey data on parameters set by petitioner’s project development teams.

The process involves three main components: an acoustic sound source, a receiver cable (sometimes referred to as the streamer), and technology to record the data. The acoustic sound source is a carefully timed and positioned man-made source signal. It typically consists of an array of 36 acoustic elements tuned to a given frequency and programed to fire simultaneously (i.e., within one or two milliseconds). The acoustic sound source is placed in the water and towed behind the vessel.

The receiver cables trail behind the vessel, typically at a depth of 10 to 15 meters below the surface of the water. The streamers are long, small-diameter tubes that contain listening devices called hydrophones, which detect the reflected seismic energy from the acoustic sound source. Each streamer is approximately 12 kilometers long, consists of segments between 50 and 200 meters long, and contains thousands of hydrophones.

During a typical marine seismic survey, the acoustic sound source fires a pulse of mechanical energy, forced downward into the seabed, generating a complex sequence of mechanical waves. The pulses reflect off rock strata at varying frequencies. The mechanical waves propagated through the subsurface are reflected from the seabed back up to the streamer, where they are recorded by

the pressure-sensitive hydrophones.4 The firing of the pulse is repeated every 10 to 20 seconds as the survey is conducted. The hydrophones record the reflected waves by converting pressure oscillations to electronic data, which is transmitted to the vessel through the streamer cable and recorded onto magnetic field tapes. Two sets of tapes are usually produced: one set containing the raw seismic data and another containing the raw seismic data combined and coordinated with the navigation or location data.

The surveyed area typically spans thousands of square kilometers, and the seismic surveys can take three months or more to complete.5 A typical 3-D seismic survey6 collects approximately 1,750 gigabytes of data every 24 hours.

4 The acoustic sound source produces an audible noise when it is fired, but that noise is not recorded during the collection of seismic data.

5 Some surveys were conducted in multiple phases. For example, petitioner’s survey of the Mississippi Canyon area of the U.S. Gulf of Mexico, a joint venture with two other seismic contractors, was performed over six phases that took place during 1999 and 2000.

6 A 3-D survey collects data through multiple acoustic sound sources and multiple streamers placed so that the resulting data can form a three-dimensional picture of the subsurface. In contrast, a 2-D survey involves a single acoustic sound source and a single streamer, and the reflected data reflects a flat “slice” of the earth. Placing multiple sound sources and multiple streamers effectively produces slices so close together as to generate a three-dimensional image.

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TGS-NOPEC Geophysical Company and Subsidiaries v. Commissioner, 155 T.C. No. 3 (tax 2020).

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