by L. Paul Tybor New Mexico Bureau of Mines and Mineral Resources Open File Report No. OF 197
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1 New Mexico Bureau of Mines and Mineral Resources Open File Report No. OF 197 HYDROCARBON SOURCE-ROCK EVALUATION STUDY, COCKRELL NO. 1 STATE WELL LUNA COUNTYl NEW MEXICO GeoChern Laboratories, Inc. by L. Paul Tybor Houston, Texas 'May
2 GEOCHEMICAL ANALYSES CRUDE oil source ROCK CRUDE OIL CHARACTERIZATION SOURCE ROCK EVALUATION GEOCHEMICAL PROSPECTING 1143-C BRITTMOORE ROAD 0 HOUSTON, TEXAS / Mr. Clayton S. Valder Marshall R. Young Oil Co. 750 West Fifth Street Fort Worth, Texas May 17, 1982 Dear Mr. Valder: Enclosed please find the results of the organic geochemical analyses performed on well cutting samples from the Cockrell 411 Stat eh?&, located in Luna County, New Mexico. I\ Upon arrival at the lab, the samples were assigned the GeoChem Job Number 2288, and were submitted to the following analytical program: Type of Analysis - Table Total organic carbon determination and brief lithological description... I Visual kerogen assessment...;ii Due to the organic-lean nature of these rocks, as determined from the organic carbon screen analyses performed, pyrolysis analysis was not carried out on any of these samples. A. Thermal Maturity DISCUSSION OF THE RESULTS The thermal maturity of the sediments from the analyzed well interval ranges from an immature Maturation Index Stage 1+ to 2- at feet, within the Lobo, to a moderately mature Maturation Index Stage to 2+ at feet, within the El Paso. Kerogen assessment was performed on the smpie from the underlying Bliss Sandstone, however it appears that this sample is comprised predominantly of thermally immature cavings. Consequently, no maturity data is available for this unit, however by extrapolating from the overlying moderately mature rocks, it can be safely assumed that these Cambrian rocks have attained at least a moderately mature maturation level.
3 Mr. Clayton Valder -2- May 17, 1982 The sediments at feet are thermally immature and prospective for only biogenic methane gas. Frm feet to feet, the rocks are moderately mature and considered-to be within The oil window. B. Hydrocarbon Source Characterization The rocks analyzed from well interval feet to feet are organic-lean with poor hydrocarbon source yharacteristics. If the moderately mature rocks analyzed in this well were encountered at an organically-rich position elsewhere in the basin, then significant hydrocarbon generation could have occurred. Should you have any questions concerning this data assistance to you, please feel free to contact us. or if we can be of further Yours truly, st Enclosures
4 Table I SCREENANALYSIS SUMMARY GeoChem We1 1 Organic Total Samp 1 e Interval Brief Lithological Description Carbon Number (Feet) (X of Rock) i Shale, grayish red. Shale, grayish red. Composite: Shale and siltstone, Pale red. Limestone, pinkish gray. Limestone, brownish gray. Limestone, light gray. Dolomite, light gray. Limestone, light gray. Limestone, pinkish gray. Dolomite, pinkish gray. Composite: Limestone and sandstone / /
5
6 New Me.xico Bureau of Mine's and Mineral Resources Open'File Report No. OF I HYDROCARBON SOURCE-ROCK EVALUATION STUDY, COCKRELL NO. 1 STATE-1,349 WELL LUNA COUNTY, NEW MEXICO by L. Paul Ty,bor GeoChem Laboratories, InC. Houston, Texas May 17,.1982
7 GEoc"EM'cAL CRUDE OIL-SOURCE ROCK CORRELATION CRUDE OEOCnEMICAL OIL CHARACTERIZATION prospectino SOURCE ROCK.EVALUATION 1143-C BRIRMOORE ROAD 0 HOUSTON, TEXAS /467~7011 Nay 17, 1982 Mr. Clayton S. Valder Marshall R. Young Oil Co. 750 West Fifth Street Fort Worth, Texas Dear Mr.'Valder:.. Enclosed please find the results of the organic gepchemical analyses performed.:. ' on well cutting samples from the Cockrell #l.stat*x6eil, located in Luna County, 'New Mexico. Upon arrival at the lab, the samples were assigned the GeoChem Job Number 2288, and were submitted to the following analytical program: Type of Analysis - Table Total organic carbon determination and brief lithological description... I Visual kerogen assessment...'.ii Due to. the organic-lean nature of these rocks; as determined frm the organic carbon screen analyses performed, pyrolysis analysis was not carried out on any of these samples. A. Thermal Maturity DISCUSSION OF THE RESULTS The thermal maturity of the sediments fr& the analyzed well interval ranges from an immature Maturation Index Stage 1+ to.2- at feet, within the Lobo, to a moderately mature Maturation Index Stage i to 2+ at feet, within the El Paso. Kerogen assessment was performed on the sbpie fron the underlying Bliss Sandstone, however it appears that this sample is comprised predominantly of.thermally immature cavings. Consequently, no maturity data is available for this unit, however by extrapolating from the.overlying moderately mature rocks, it can be safely assumed that these Cambrian rocks have attained at 1east.a moderately mature maturation level.
8 Mr. Clayton Valder May 17, 1982.! The sediments at feet are thermally immature and prospective for only biogenic methane gas. Fran feet to feet, the rocks are moderately mature and considered-to be within The oil window. B. Hydrocarbon Source Characterization The rocks analyzed from well interval feet to feet are org.anic-lean with poor hydrocarbon source yharacteristics. If the moderately mature rocks analyzed in this well were encountered at an organically-rich position elsewhere in the basin, then significant hydrocarbon generation could have occurred. Should you have any questions concerning this data or if we can be of further assistance to you, please feel free to contact us. Yours truly, Lator GEOCHEM LABORAT ORES, INC. st- Enclosures
9 Table I - SCREENANALYSIS SUMMARY GeoChem Sample Number.. We1 1 Intervi I1 (Feet I Brief Lithological Description Total Organic Carbon (% of Rock) Shale, grayish red. Shale, grayish red. Composite: Shale and siltstone, Pale red. Limestone, pinkish gray / Limestone, brownish gray Limestone, light gray Dolomite, light gray. Limestone, light gray.. Limestone, pinkish gray / Dolomite, pinkish gray. Composite: Limestone and sandstone
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