Natland, James H; Adamson, Andrew C; Laverne, Christine; Melson, William G; O'Hearn, Timothy (1983): (Table 6) Geochemistry of plagioclases at DSDP Legs 69-70 Holes [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.817006, In supplement to: Natland, JH et al. (1983): A compositionally nearly steady-state magma chamber at the Costa Rica Rift: Evidence from basalt glass and mineral data, Deep Sea Drilling Project Sites 501, 504, and 505. In: Cann, JR; Langseth, MG; Honnorez, J; Von Herzen, RP; White, SM; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 69, 811-858, https://doi.org/10.2973/dsdp.proc.69.154.1983
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Median Latitude: 1.502860 * Median Longitude: -83.754200 * South-bound Latitude: 1.226800 * West-bound Longitude: -83.790000 * North-bound Latitude: 1.920000 * East-bound Longitude: -83.730000
Date/Time Start: 1979-09-24T00:00:00 * Date/Time End: 1979-12-04T00:00:00
Minimum Elevation: -3537.0 m * Maximum Elevation: -3458.0 m
Event(s):
69-504A * Latitude: 1.226800 * Longitude: -83.732500 * Date/Time: 1979-09-24T00:00:00 * Elevation: -3458.0 m * Penetration: 277 m * Recovery: 207 m * Campaign: Leg69 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL)
69-504B * Latitude: 1.227200 * Longitude: -83.730200 * Date/Time: 1979-10-07T00:00:00 * Elevation: -3460.0 m * Penetration: 489 m * Recovery: 262 m * Campaign: Leg69 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL)
69-505 * Latitude: 1.913300 * Longitude: -83.790000 * Date/Time: 1979-09-29T00:00:00 * Elevation: -3537.0 m * Penetration: 242 m * Recovery: 187.1 m * Location: North Pacific/GRABEN * Campaign: Leg69 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 26 cores; 223 m cored; 0 m drilled; 83.9 % recovery
Comment:
Structural formulae calculated on the basis of 32 oxygens.
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Latitude of event | Latitude | ||||
3 | Longitude of event | Longitude | ||||
4 | Elevation of event | Elevation | m | |||
5 | Sample code/label | Sample label | Natland, James H | DSDP/ODP/IODP sample designation | ||
6 | Piece | Piece | Natland, James H | |||
7 | Comment | Comment | Natland, James H | |||
8 | Comment 2 (continued) | Comm 2 | Natland, James H | |||
9 | Silicon dioxide | SiO2 | % | Natland, James H | Electron microprobe (EMP) | |
10 | Aluminium oxide | Al2O3 | % | Natland, James H | Electron microprobe (EMP) | |
11 | Iron oxide, FeO | FeO | % | Natland, James H | Electron microprobe (EMP) | Total iron |
12 | Magnesium oxide | MgO | % | Natland, James H | Electron microprobe (EMP) | |
13 | Calcium oxide | CaO | % | Natland, James H | Electron microprobe (EMP) | |
14 | Sodium oxide | Na2O | % | Natland, James H | Electron microprobe (EMP) | |
15 | Potassium oxide | K2O | % | Natland, James H | Electron microprobe (EMP) | |
16 | Total | Total | % | Natland, James H | Electron microprobe (EMP) | |
17 | Silicon | Si | # of ions | Natland, James H | Calculated based on oxygen number | |
18 | Aluminium | Al | # of ions | Natland, James H | Calculated based on oxygen number | |
19 | Iron 2+ and 3+ | Fe | # of ions | Natland, James H | Calculated based on oxygen number | |
20 | Magnesium | Mg | # of ions | Natland, James H | Calculated based on oxygen number | |
21 | Calcium | Ca | # of ions | Natland, James H | Calculated based on oxygen number | |
22 | Sodium | Na | # of ions | Natland, James H | Calculated based on oxygen number | |
23 | Potassium | K | # of ions | Natland, James H | Calculated based on oxygen number | |
24 | Anorthite | An | % | Natland, James H | CIPW Norm | |
25 | Type | Type | Natland, James H | Crystal | ||
26 | Group | Group | Natland, James H | see reference(s) | Glass group |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1775 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Sample label | 6 Piece | 7 Comment | 8 Comm 2 | 9 SiO2 [%] | 10 Al2O3 [%] | 11 FeO [%] | 12 MgO [%] | 13 CaO [%] | 14 Na2O [%] | 15 K2O [%] | 16 Total [%] | 17 Si [# of ions] | 18 Al [# of ions] | 19 Fe [# of ions] | 20 Mg [# of ions] | 21 Ca [# of ions] | 22 Na [# of ions] | 23 K [# of ions] | 24 An [%] | 25 Type | 26 Group |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-7-2,98-102 | 466 | Analyst = Adamson | 47.52 | 34.32 | 0.32 | 0.00 | 18.27 | 0.86 | 0.00 | 101.29 | 8.621 | 7.339 | 0.048 | 0.000 | 3.551 | 0.301 | 0.000 | 92.2 | Phenocryst (core) | B | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-7-2,98-102 | 466 | Analyst = Adamson | 47.05 | 32.96 | 0.45 | 0.00 | 17.50 | 1.34 | 0.00 | 99.30 | 8.712 | 7.195 | 0.069 | 0.000 | 3.473 | 0.481 | 0.000 | 87.8 | Phenocryst (core) | B | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-7-3,27-30 | 476 | Analyst = Adamson | 47.60 | 32.97 | 0.44 | 0.00 | 17.96 | 1.15 | 0.00 | 100.12 | 8.742 | 7.139 | 0.068 | 0.000 | 3.535 | 0.408 | 0.000 | 89.7 | Phenocryst (core) | B | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-7-3,27-30 | 476 | Analyst = Adamson | 45.96 | 33.20 | 0.37 | 0.00 | 18.24 | 0.86 | 0.00 | 98.63 | 8.585 | 7.311 | 0.057 | 0.000 | 3.651 | 0.310 | 0.000 | 82.2 | Phenocryst (core) | B | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-13-3,66-69 | 791 | Analyst = Adamson | 48.37 | 32.95 | 0.39 | 0.00 | 17.45 | 1.21 | 0.00 | 100.37 | 8.834 | 7.096 | 0.060 | 0.000 | 3.414 | 0.427 | 0.000 | 88.8 | Phenocryst (core) | B | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-13-3,66-69 | 791 | Analyst = Adamson | 49.18 | 31.82 | 0.69 | 0.00 | 16.54 | 1.94 | 0.00 | 100.18 | 9.002 | 6.868 | 0.106 | 0.000 | 3.244 | 0.687 | 0.000 | 82.5 | Phenocryst (rim) | B | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-13-3,66-69 | 791 | Analyst = Adamson | Analysis is somewhat suspect | 53.07 | 31.04 | 1.10 | 0.29 | 15.15 | 2.90 | 0.00 | 103.54 | 9.361 | 6.455 | 0.162 | 0.076 | 2.863 | 0.992 | 0.000 | 74.3 | Phenocryst (rim) | B |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-13-3,66-69 | 791 | Analyst = Adamson | Analysis is somewhat suspect | 53.12 | 27.03 | 1.72 | 1.21 | 13.17 | 3.43 | 0.09 | 99.76 | 9.716 | 5.828 | 0.262 | 0.329 | 2.581 | 1.215 | 0.021 | 68.0 | Microlite | B |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-16-1,4-7 | 956 | Analyst = Adamson | Analysis is somewhat suspect | 45.43 | 30.60 | 0.35 | 0.00 | 16.73 | 1.55 | 0.00 | 94.66 | 8.826 | 7.010 | 0.058 | 0.000 | 3.483 | 0.585 | 0.000 | 85.6 | Phenocryst (core) | D |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-16-1,4-7 | 956 | Analyst = Adamson | 46.92 | 32.49 | 0.45 | 0.22 | 17.52 | 1.09 | 0.00 | 98.69 | 8.738 | 7.134 | 0.069 | 0.061 | 3.496 | 0.392 | 0.000 | 88.8 | Phenocryst (core) | D | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-16-1,4-7 | 956 | Analyst = Adamson | 47.13 | 33.37 | 0.40 | 0.00 | 17.81 | 1.14 | 0.00 | 98.85 | 8.767 | 7.098 | 0.062 | 0.000 | 3.551 | 0.412 | 0.000 | 89.6 | Phenocryst (core) | D | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-16-1,4-7 | 956 | Analyst = Adamson | 46.86 | 33.13 | 0.43 | 0.00 | 17.82 | 1.15 | 0.00 | 99.38 | 8.667 | 7.224 | 0.066 | 0.000 | 3.531 | 0.413 | 0.000 | 89.5 | Phenocryst (core) | D | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-16-1,4-7 | 956 | Analyst = Adamson | Analysis is somewhat suspect | 52.45 | 28.43 | 1.60 | 0.23 | 13.19 | 3.98 | 0.00 | 99.89 | 9.599 | 6.134 | 0.245 | 0.063 | 2.587 | 1.413 | 0.000 | 64.7 | Microlite | D |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-16-1,4-7 | 956 | Analyst = Adamson | 46.92 | 33.23 | 0.49 | 0.00 | 18.06 | 1.41 | 0.00 | 100.12 | 8.642 | 7.216 | 0.075 | 0.000 | 3.564 | 0.505 | 0.000 | 87.6 | Phenocryst (core) | D | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-16-1,4-7 | 956 | Analyst = Adamson | 48.74 | 33.02 | 0.47 | 0.00 | 17.77 | 1.43 | 0.00 | 101.41 | 8.828 | 7.048 | 0.072 | 0.000 | 3.450 | 0.501 | 0.000 | 87.3 | Phenocryst (core) | D | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-16-1,4-7 | 956 | Analyst = Adamson | 45.46 | 32.01 | 0.74 | 0.21 | 17.70 | 1.26 | 0.00 | 97.37 | 8.626 | 7.161 | 0.117 | 0.061 | 3.599 | 0.462 | 0.000 | 88.6 | Phenocryst (rim) | D | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-21-4,120-124 | 1254 | Analyst = Adamson | Analysis is somewhat suspect | 50.26 | 30.65 | 1.05 | 0.55 | 15.61 | 2.57 | 0.00 | 100.70 | 9.156 | 6.584 | 0.160 | 0.150 | 3.047 | 0.909 | 0.000 | 77.0 | Phenocryst (rim) | G |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-41-2,75-77 | 605 | Analyst = Adamson | 45.76 | 33.20 | 0.26 | 0.23 | 18.14 | 1.31 | 0.00 | 98.89 | 8.538 | 7.304 | 0.040 | 0.064 | 3.626 | 0.473 | 0.000 | 88.5 | Phenocryst (core) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-47-1,7-11 | 804 | Analyst = Adamson | Analysis is somewhat suspect | 44.82 | 32.78 | 0.33 | 0.00 | 17.99 | 0.92 | 0.00 | 96.84 | 8.535 | 7.359 | 0.052 | 0.000 | 3.671 | 0.338 | 0.000 | 91.6 | Phenocryst (core) | K |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-47-1,7-11 | 804 | Analyst = Adamson | Analysis is somewhat suspect | 52.29 | 22.87 | 4.42 | 1.04 | 11.66 | 4.18 | 0.03 | 96.47 | 10.003 | 5.158 | 0.707 | 0.296 | 2.389 | 1.552 | 0.000 | 60.6 | Phenocryst (rim) | K |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-47-1,7-11 | 804 | Analyst = Adamson | 45.64 | 33.01 | 0.39 | 0.00 | 18.07 | 0.96 | 0.00 | 98.08 | 8.578 | 7.312 | 0.062 | 0.000 | 3.639 | 0.351 | 0.000 | 91.2 | Phenocryst (core) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-49-1,51-54 | 922 | Analyst = Adamson | 45.96 | 32.43 | 0.32 | 0.00 | 17.61 | 1.05 | 0.00 | 97.37 | 8.580 | 7.221 | 0.050 | 0.000 | 3.564 | 0.385 | 0.000 | 90.3 | Phenocryst (core) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-49-1,51-54 | 922 | Analyst = Adamson | 49.72 | 29.45 | 0.82 | 0.00 | 14.68 | 2.82 | 0.00 | 97.07 | 9.341 | 6.522 | 0.129 | 0.000 | 2.955 | 0.831 | 0.000 | 78.1 | Microlite | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-49-1,51-54 | 922 | Analyst = Adamson | 46.47 | 32.62 | 0.38 | 0.00 | 17.62 | 1.23 | 0.00 | 98.32 | 8.696 | 7.196 | 0.059 | 0.000 | 3.532 | 0.447 | 0.000 | 88.8 | Phenocryst (core) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-49-1,51-54 | 922 | Analyst = Adamson | 46.91 | 32.45 | 0.38 | 0.00 | 17.23 | 1.34 | 0.00 | 98.30 | 8.764 | 7.148 | 0.059 | 0.000 | 3.449 | 0.484 | 0.000 | 87.7 | Phenocryst (core) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-49-1,51-54 | 922 | Analyst = Adamson | 46.68 | 32.61 | 0.34 | 0.00 | 17.96 | 1.19 | 0.00 | 98.77 | 8.700 | 7.165 | 0.053 | 0.000 | 3.586 | 0.428 | 0.000 | 89.3 | Phenocryst (core) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-49-1,51-54 | 1061 | Analyst = Adamson | 51.13 | 28.88 | 0.99 | 0.27 | 13.11 | 3.65 | 0.00 | 97.97 | 9.508 | 6.333 | 0.154 | 0.060 | 2.612 | 1.317 | 0.000 | 66.5 | Microlite | M | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-49-1,51-54 | 1061 | Analyst = Adamson | Analysis is somewhat suspect | 50.15 | 21.53 | 4.06 | 4.51 | 14.89 | 2.88 | 0.00 | 98.02 | 9.570 | 4.845 | 0.648 | 1.282 | 3.045 | 1.067 | 0.000 | 74.1 | Phenocryst (rim) | M |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-49-1,51-54 | 1061 | Analyst = Adamson | 52.92 | 28.22 | 0.93 | 0.33 | 12.52 | 4.62 | 0.00 | 99.54 | 9.682 | 6.087 | 0.142 | 0.091 | 2.454 | 1.640 | 0.000 | 59.9 | Microlite | M | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-56-1,2-4 | 1099 | Analyst = Laverne | 56.10 | 27.06 | 0.99 | 0.10 | 8.71 | 5.91 | 0.10 | 98.98 | 10.190 | 5.796 | 0.150 | 0.027 | 1.696 | 2.082 | 0.000 | 44.9 | Microlite | M | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-56-1,2-4 | 1099 | Analyst = Laverne | 51.67 | 30.00 | 0.53 | 0.23 | 11.86 | 3.99 | 0.00 | 98.28 | 9.515 | 6.514 | 0.082 | 0.063 | 2.341 | 1.425 | 0.000 | 62.2 | Microlite | M | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-56-1,2-4 | 1099 | Analyst = Laverne | 52.52 | 30.25 | 0.74 | 0.31 | 12.30 | 3.51 | 0.03 | 99.66 | 9.537 | 6.477 | 0.112 | 0.084 | 2.394 | 1.236 | 0.007 | 66.0 | Microlite | M | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-56-1,2-4 | 1189 | Analyst = Laverne | 52.76 | 29.38 | 0.79 | 0.19 | 12.21 | 4.30 | 0.00 | 99.62 | 9.610 | 6.310 | 0.120 | 0.052 | 2.383 | 1.519 | 0.000 | 61.1 | Microlite | M | |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-2-1,25-28 | 107 | Analyst = Adamson | 50.33 | 30.74 | 0.54 | 0.00 | 15.47 | 2.28 | 0.00 | 99.35 | 9.242 | 6.656 | 0.083 | 0.000 | 3.043 | 0.810 | 0.000 | 79.0 | Phenocryst (core) | P | |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-2-1,25-28 | 107 | Analyst = Adamson | 50.34 | 31.05 | 0.44 | 0.00 | 15.81 | 2.45 | 0.00 | 100.09 | 9.191 | 6.684 | 0.067 | 0.000 | 3.093 | 0.867 | 0.000 | 78.1 | Phenocryst (core) | P | |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-2-2,100-103 | 142 | Analyst = Adamson | 45.62 | 34.30 | 0.22 | 0.00 | 18.70 | 0.76 | 0.00 | 99.60 | 8.446 | 7.485 | 0.034 | 0.000 | 3.710 | 0.274 | 0.000 | 93.1 | Phenocryst (core) | P | |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-2-2,100-103 | 142 | Analyst = Adamson | 45.17 | 34.32 | 0.28 | 0.00 | 19.01 | 0.83 | 0.00 | 99.61 | 8.382 | 7.508 | 0.044 | 0.000 | 3.780 | 0.299 | 0.000 | 92.7 | Phenocryst (core) | P | |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-2-2,100-103 | 142 | Analyst = Adamson | Analysis is somewhat suspect | 51.20 | 21.33 | 6.44 | 3.24 | 14.93 | 2.43 | 0.15 | 99.68 | 9.664 | 4.746 | 1.017 | 0.911 | 3.020 | 0.890 | 0.020 | 77.2 | Phenocryst (rim) | P |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-2-2,100-103 | 142 | Analyst = Adamson | Analysis is somewhat suspect | 55.81 | 26.70 | 1.60 | 0.00 | 11.38 | 4.85 | 0.00 | 100.48 | 10.055 | 5.672 | 0.241 | 0.000 | 2.198 | 1.693 | 0.000 | 56.5 | Microlite | P |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-2-2,100-103 | 142 | Analyst = Adamson | 45.88 | 34.12 | 0.26 | 0.00 | 18.81 | 0.95 | 0.00 | 100.01 | 8.468 | 7.424 | 0.041 | 0.000 | 3.719 | 0.337 | 0.000 | 91.7 | Phenocryst (core) | P | |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-2-2,100-103 | 142 | Analyst = Adamson | 46.58 | 32.89 | 0.37 | 0.00 | 17.56 | 1.34 | 0.00 | 98.71 | 8.682 | 7.221 | 0.057 | 0.000 | 3.506 | 0.484 | 0.000 | 87.9 | Phenocryst (core) | P | |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-3-1,109-112 | 175 | Analyst = Adamson | Analysis is somewhat suspect | 46.75 | 31.27 | 0.42 | 0.00 | 16.54 | 1.60 | 0.00 | 96.59 | 8.883 | 7.005 | 0.067 | 0.000 | 3.367 | 0.589 | 0.000 | 85.1 | Phenocryst (core) | P |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-3-1,109-112 | 175 | Analyst = Adamson | Analysis is somewhat suspect | 45.66 | 32.35 | 0.32 | 0.00 | 17.43 | 1.15 | 0.00 | 96.92 | 8.667 | 7.239 | 0.051 | 0.000 | 3.545 | 0.424 | 0.000 | 89.3 | Phenocryst (core) | P |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-5-1,50-60 | 199 | Analyst = Adamson | 46.84 | 33.12 | 0.41 | 0.00 | 17.70 | 1.19 | 0.00 | 99.26 | 8.679 | 7.234 | 0.063 | 0.000 | 3.514 | 0.428 | 0.000 | 89.1 | Phenocryst (core) | P | |
69-505 | 1.9133 | -83.7900 | -3537 | 69-505-26-1,3-5 | 93 | Analyst = Adamson | 47.51 | 32.78 | 0.40 | 0.00 | 17.58 | 1.27 | 0.00 | 99.54 | 8.768 | 7.132 | 0.062 | 0.000 | 3.476 | 0.456 | 0.000 | 88.4 | Phenocryst (core) | ||
69-505 | 1.9133 | -83.7900 | -3537 | 69-505-26-1,3-5 | 93 | Analyst = Adamson | 48.44 | 32.41 | 0.34 | 0.00 | 17.36 | 1.60 | 0.00 | 100.15 | 8.876 | 7.002 | 0.052 | 0.000 | 3.408 | 0.570 | 0.000 | 85.7 | Phenocryst (core) | ||
69-505 | 1.9133 | -83.7900 | -3537 | 69-505-26-1,3-5 | 93 | Analyst = Adamson | 48.58 | 31.55 | 0.32 | 0.00 | 16.44 | 1.87 | 0.00 | 98.76 | 9.004 | 6.894 | 0.051 | 0.000 | 3.265 | 0.672 | 0.000 | 82.9 | Phenocryst (core) | ||
69-505 | 1.9133 | -83.7900 | -3537 | 69-505-26-1,3-5 | 93 | Analyst = Adamson | 50.32 | 31.13 | 0.50 | 0.00 | 15.32 | 2.45 | 0.00 | 99.85 | 9.197 | 6.706 | 0.076 | 0.000 | 3.001 | 0.869 | 0.000 | 77.5 | Microlite | ||
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-21-4,120-124 | 1254 | Analyst = Adamson | 46.63 | 33.30 | 0.46 | 0.00 | 18.01 | 1.13 | 0.00 | 99.53 | 8.629 | 7.264 | 0.071 | 0.000 | 3.572 | 0.406 | 0.000 | 89.8 | Phenocryst (core) | G | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-21-4,120-124 | 1254 | Analyst = Adamson | 48.08 | 32.56 | 0.30 | 0.00 | 16.97 | 1.53 | 0.00 | 99.42 | 8.852 | 7.065 | 0.047 | 0.000 | 3.348 | 0.544 | 0.000 | 86.0 | Phenocryst (core) | G | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-21-4,120-124 | 1378 | Analyst = Adamson | 45.32 | 32.68 | 0.36 | 0.00 | 17.87 | 1.10 | 0.00 | 97.34 | 8.584 | 7.298 | 0.056 | 0.000 | 3.627 | 0.404 | 0.000 | 90.0 | Phenocryst (core) | G | |
69-504B | 1.2272 | -83.7302 | -3460 | 69-504B-29-1,11-14 | 1560 | Analyst = Adamson | Analysis is somewhat suspect | 49.40 | 28.94 | 2.24 | 0.75 | 12.52 | 2.46 | 0.00 | 98.28 | 9.226 | 6.372 | 0.350 | 0.209 | 2.903 | 0.890 | 0.000 | 76.5 | Microlite | H |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-33-2,48-52 | 207 | Analyst = Laverne | Analysis is somewhat suspect | 52.06 | 29.40 | 0.69 | 0.34 | 13.21 | 3.62 | 0.13 | 99.45 | 9.527 | 6.344 | 0.106 | 0.093 | 2.591 | 1.285 | 0.000 | 66.8 | Microlite | I |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-33-2,48-52 | 207 | Analyst = Laverne | Analysis is somewhat suspect | 54.47 | 27.52 | 1.12 | 0.16 | 11.55 | 4.91 | 0.01 | 99.74 | 9.908 | 5.902 | 0.170 | 0.043 | 2.251 | 1.732 | 0.000 | 56.5 | Microlite | I |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-36-2,121-123 | 314 | Analyst = Adamson | Analysis is somewhat suspect | 52.73 | 27.98 | 1.26 | 0.00 | 12.52 | 4.29 | 0.00 | 98.78 | 9.722 | 6.081 | 0.194 | 0.000 | 2.473 | 1.534 | 0.000 | 61.7 | Microlite | J |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-36-2,121-123 | 314 | Analyst = Adamson | Analysis is somewhat suspect | 54.99 | 26.77 | 1.27 | 0.00 | 10.87 | 5.29 | 0.00 | 99.19 | 10.035 | 5.759 | 0.194 | 0.000 | 2.125 | 1.872 | 0.000 | 53.2 | Microlite | J |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-36-2,121-123 | 314 | Analyst = Adamson | 48.84 | 30.18 | 0.55 | 0.00 | 15.44 | 2.64 | 0.00 | 97.65 | 9.161 | 6.673 | 0.086 | 0.000 | 3.103 | 0.960 | 0.000 | 76.4 | Phenocryst (core) | J | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-37-1,15-17 | 342 | Analyst = Adamson | 49.11 | 30.46 | 0.55 | 0.00 | 15.38 | 2.15 | 0.00 | 97.65 | 9.184 | 6.715 | 0.086 | 0.000 | 3.082 | 0.781 | 0.000 | 79.8 | Phenocryst (rim) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-37-2,118-120 | 383 | Analyst = Adamson | 46.77 | 32.50 | 0.53 | 0.00 | 17.38 | 1.40 | 0.00 | 98.58 | 8.723 | 7.146 | 0.082 | 0.000 | 3.473 | 0.507 | 0.000 | 87.3 | Phenocryst (core) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-37-2,118-120 | 383 | Analyst = Adamson | 52.15 | 29.12 | 1.08 | 0.00 | 13.41 | 3.55 | 0.00 | 99.30 | 9.563 | 6.296 | 0.165 | 0.000 | 2.635 | 1.261 | 0.000 | 67.6 | Phenocryst (rim) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-37-2,118-120 | 383 | Analyst = Adamson | Analysis is somewhat suspect | 50.59 | 28.65 | 1.05 | 0.81 | 14.76 | 2.76 | 0.00 | 98.64 | 9.389 | 6.268 | 0.163 | 0.224 | 2.934 | 1.001 | 0.000 | 74.6 | Phenocryst (rim) | K |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-37-3,49-52 | 397 | Analyst = Laverne | 48.07 | 33.56 | 0.25 | 0.19 | 16.94 | 1.57 | 0.00 | 100.65 | 8.757 | 7.208 | 0.038 | 0.052 | 3.307 | 0.555 | 0.000 | 85.6 | Phenocryst (core) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-40-1,37-39 | 507 | Analyst = Laverne | 53.17 | 28.15 | 0.80 | 0.13 | 11.73 | 4.71 | 0.01 | 98.69 | 9.771 | 6.100 | 0.123 | 0.036 | 2.310 | 1.679 | 0.002 | 57.9 | Microlite | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-40-1,37-39 | 507 | Analyst = Laverne | 51.50 | 30.30 | 0.78 | 0.25 | 14.70 | 3.43 | 0.00 | 100.95 | 9.327 | 6.470 | 0.118 | 0.067 | 2.853 | 1.205 | 0.000 | 70.3 | Microlite | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-40-2,89-91 | 533 | Analyst = Adamson | 47.28 | 31.88 | 0.34 | 0.23 | 16.49 | 1.84 | 0.00 | 98.06 | 8.839 | 7.025 | 0.053 | 0.064 | 3.304 | 0.668 | 0.000 | 83.2 | Phenocryst (core) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-40-2,89-91 | 533 | Analyst = Adamson | 47.18 | 32.24 | 0.40 | 0.00 | 17.13 | 1.46 | 0.00 | 98.42 | 8.805 | 7.093 | 0.063 | 0.000 | 3.425 | 0.473 | 0.000 | 87.9 | Phenocryst (core) | K | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-58-1,35-38 | 1192 | Analyst = Adamson | 48.99 | 31.30 | 0.49 | 0.28 | 15.80 | 2.13 | 0.00 | 99.05 | 9.051 | 6.817 | 0.084 | 0.078 | 3.128 | 0.763 | 0.000 | 80.4 | Phenocryst (core) | M | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-61-3,1-4 | 1315 | Analyst = Adamson | 45.49 | 33.25 | 0.49 | 0.00 | 18.29 | 0.99 | 0.00 | 98.50 | 8.517 | 7.340 | 0.076 | 0.000 | 3.669 | 0.359 | 0.000 | 91.1 | Phenocryst (core) | N | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-61-3,1-4 | 1315 | Analyst = Adamson | 46.65 | 32.49 | 0.30 | 0.00 | 17.37 | 1.19 | 0.00 | 98.00 | 8.741 | 7.178 | 0.048 | 0.000 | 3.487 | 0.432 | 0.000 | 89.0 | Phenocryst (core) | N | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-61-3,1-4 | 1315 | Analyst = Adamson | 46.80 | 32.66 | 0.50 | 0.00 | 17.92 | 0.95 | 0.00 | 98.84 | 8.712 | 7.167 | 0.078 | 0.000 | 3.574 | 0.344 | 0.000 | 91.2 | Phenocryst (core) | N | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-61-3,1-4 | 1315 | Analyst = Adamson | 46.31 | 33.24 | 0.40 | 0.00 | 17.97 | 0.98 | 0.00 | 98.90 | 8.619 | 7.294 | 0.061 | 0.000 | 3.583 | 0.353 | 0.000 | 91.0 | Phenocryst (core) | N | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-63-4,7-10 | 1392 | Analyst = Laverne | 51.21 | 30.15 | 0.67 | 0.24 | 13.62 | 3.27 | 0.00 | 99.17 | 9.395 | 6.522 | 0.103 | 0.066 | 2.678 | 1.163 | 0.000 | 69.7 | Microlite | N | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-63-4,65-69 | 1398 | Analyst = Adamson | 44.86 | 33.65 | 0.35 | 0.00 | 18.59 | 0.60 | 0.00 | 98.04 | 8.444 | 7.466 | 0.054 | 0.000 | 3.749 | 0.220 | 0.000 | 94.5 | Phenocryst (core) | N | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-64-3,87-92 | 1450 | Analyst = Laverne | 51.19 | 30.80 | 0.58 | 0.33 | 13.95 | 3.09 | 0.01 | 99.95 | 9.319 | 6.611 | 0.088 | 0.090 | 2.721 | 1.091 | 0.002 | 71.4 | Microlite | N | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-64-3,87-92 | 1450 | Analyst = Laverne | 50.20 | 30.39 | 0.43 | 0.33 | 13.71 | 2.98 | 0.00 | 98.03 | 9.308 | 6.644 | 0.067 | 0.091 | 2.724 | 1.072 | 0.000 | 71.8 | Microlite | N | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-66-2,106-109 | 1519 | Analyst = Adamson | 51.51 | 29.18 | 0.95 | 0.24 | 13.90 | 3.40 | 0.00 | 99.18 | 9.475 | 6.327 | 0.146 | 0.066 | 2.740 | 1.214 | 0.000 | 61.3 | Microlite | O | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-66-2,106-109 | 1519 | Analyst = Adamson | 49.48 | 30.65 | 0.55 | 0.22 | 15.39 | 2.86 | 0.00 | 99.16 | 9.141 | 6.676 | 0.086 | 0.061 | 3.047 | 1.023 | 0.000 | 74.9 | Microlite | O | |
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-69-1,106-112 | 1548 | Analyst = Adamson | 52.05 | 30.41 | 0.98 | 0.34 | 14.73 | 3.12 | 0.00 | 101.62 | 9.357 | 6.446 | 0.148 | 0.090 | 2.836 | 1.087 | 0.000 | 72.3 | Microlite | ||
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-69-1,106-112 | 1548 | Analyst = Adamson | 49.47 | 25.04 | 2.29 | 3.43 | 14.71 | 2.15 | 0.00 | 97.09 | 9.388 | 5.604 | 0.364 | 0.970 | 2.991 | 0.792 | 0.000 | 79.1 | Phenocryst (core) | ||
70-504B | 1.2270 | -83.7300 | -3460 | 70-504B-69-1,106-112 | 1548 | Analyst = Adamson | 46.66 | 32.32 | 0.40 | 0.00 | 17.27 | 1.57 | 0.00 | 98.22 | 8.740 | 7.138 | 0.063 | 0.000 | 3.466 | 0.570 | 0.000 | 85.9 | Phenocryst (core) | ||
69-504A | 1.2268 | -83.7325 | -3458 | 69-504A-6-3,12-15 | 48 | Analyst = Adamson | 54.38 | 29.18 | 1.46 | 0.00 | 12.30 | 4.09 | 0.00 | 102.10 | 9.696 | 6.134 | 0.217 | 0.000 | 2.483 | 1.414 | 0.000 | 63.7 | Microlite | A? | |
69-504A | 1.2268 | -83.7325 | -3458 | 69-504A-7-1,50-53 | 65 | Analyst = Adamson | 47.18 | 32.54 | 0.43 | 0.00 | 17.53 | 1.32 | 0.00 | 99.01 | 8.763 | 7.122 | 0.066 | 0.000 | 3.488 | 0.474 | 0.000 | 88.0 | Phenocryst (core) | A? | |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-2-1,25-28 | 107 | Analyst = Adamson | 55.90 | 25.48 | 1.41 | 0.00 | 9.98 | 5.71 | 0.00 | 98.47 | 10.254 | 5.509 | 0.216 | 0.000 | 1.961 | 2.030 | 0.000 | 49.1 | Microlite | P | |
69-505B | 1.9200 | -83.7883 | -3507 | 69-505B-2-1,25-28 | 107 | Analyst = Adamson | 50.79 | 28.82 | 0.93 | 0.26 | 14.18 | 3.20 | 0.00 | 98.17 | 9.449 | 6.321 | 0.145 | 0.071 | 2.827 | 1.153 | 0.000 | 71.0 | Phenocryst (rim) | P |