skip all navigation
skip banner links

Data Repository

Find a Repository Dataset (You can also browse listings by Author or Year/Number.)

— or enter any of these search parameters:

  

Data in this repository supplements published papers in our publications. Please refer to both the published material and the repository documentation before using this data. Please cite repository data as shown in each repository listing.

Please direct comments or requests regarding these datasets to either the author(s) or the Webmaster.

 Pub-Info 

2018006

McLemore, V.T.; Smith, A.; Riggins, A.M.; Dunbar N.; Frempong, K.B.; Heizler, M.T., 2018, Characterization and origin of episyenites in the southern Caballo Mountains, Sierra County, NM, in: Las Cruces Country III, Mack, Greg H.; Hampton, Brian A.; Ramos, Frank C.; Witcher, James C.; Ulmer-Scholle, Dana S., ed(s), New Mexico Geological Society, Guidebook, 69th Field Conference, v. 69, pp. 207-216.  https://doi.org/10.56577/FFC-69.207
Repository: 2018006 < https://nmgs.nmt.edu/repository/index.cfml?rid=2018006 >

Data Description:

  • APPENDIX 1. Mines and prospects in the southern Caballo Mountains mining district, Sierra County. Mine Id Numbers are from the New Mexico Mines database. Latitude and longitude are in NAD27.
  • APPENDIX 2. Color geologic maps and photographs of episyenites.
    • FIGURE A2-1. Geologic map of the Apache Gap episyenites area, southern Caballo Mountains.
    • FIGURE A2-2. Geologic map of the Southern Red Hills episyenites area, southern Caballo Mountains.
    • FIGURE A2-3. Episyenite (red) in contact with the Caballo granite.
    • FIGURE A2-4. Episyenites hosted by the Caballo granite in the Southern Red Hills, Caballo Mountains.
    • FIGURE A2-5. Red, altered K-feldspar episyenites in the basal Bliss Sandstone indicate that episyenites are no younger than Cambrian-Ordovician.
    • FIGURE A2-6. Red, altered K-feldspar episyenites in the basal Bliss Sandstone indicate that episyenites are no younger than Cambrian-Ordovician.
  • APPENDIX 3. Chemical analyses of episyenites and granites in the southern Caballo Mountains. Major oxides are in percent (%) and trace elements are in parts per million (ppm). Latitude and longitude are in NAD27. Na=not available. TREE=total rare earth elements. Fe2O3T=Total iron calculated as Fe2O3

Download

File Name Size Last Modified
Appendix1.xlsx 17 KB 10/12/2018 03:06:28 PM
Appendix3.xlsx 39 KB 10/12/2018 03:06:34 PM
SUPPLEMENTAL_MATERIAL.docx 20 KB 10/17/2018 02:43:02 PM
SUPPLEMENTAL_MATERIAL.pdf 367 KB 10/17/2018 02:43:21 PM
Appendix2:
FigA2-1ApacheGapcolored.jpg 1.33 MB 10/12/2018 03:05:17 PM
FigA2-2SRedHillscolored.tif 97.06 MB 10/12/2018 03:06:23 PM
FigA2-3gran_epi.JPG 6.32 MB 10/12/2018 03:05:11 PM
FigA2-4epi.JPG 5.89 MB 10/12/2018 03:05:01 PM
FigA2-5epi_clasts.JPG 6.22 MB 10/12/2018 03:04:50 PM
FigA2-6epi_clasts.JPG 5.73 MB 10/12/2018 03:04:40 PM