Cargill Township carbonatite complex, District of ... - Geology Ontario
Cargill Township carbonatite complex, District of ... - Geology Ontario Cargill Township carbonatite complex, District of ... - Geology Ontario
CARBONATITE - ALKALIC ROCK COMPLEXES: CARGILL TOWNSHIP TABLE A-4. CONTINUED. Ref. No. QZ CO OR AB LC KAL NEPH CAR NS AC TH GEH AKM FE-AK D. WO D. EN D. FS FO FA ANDR HM MT SPH PERV RU AP CC MGS FL ZR BAD H2O SUM 837 0.95 0.35 0.47 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.78 0.0 0.0 0.0 0.0 0.0 0.0 2.70 3.60 0.0 0.0 1.70 0.0 0.0 0.24 6.72 75.89 4.01 0.0 0.0 0.0 0.47 97.89 SOVITE 833 2.24 0.40 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 1.08 0.0 0.0 0.0 0.0 0.0 0.0 0.21 3.04 0.0 0.0 2.59 0.0 0.0 0.29 14.86 64.43 8.10 0.0 0.0 0.0 0.27 97.51 832 0.0 0.48 0.57 0.0 0.43 0.0 0.0 0.0 0.0 0.0 1.26 0.0 0.0 0.0 0.0 0.0 0.0 0.0 2.93 0.0 0.0 1.48 0.0 0.0 0.18 7.39 79.34 3.71 0.0 0.0 0.0 0.33 98.10 773 0.0 0.0 2.47 0.0 11.65 0.0 3.27 0.0 0.0 10.73 1.33 0.0 0.0 0.0 4.54 3.52 0.52 26.19 4.31 0.0 0.0 5.94 2.38 0.0 0.0 4.02 17.27 0.0 0.0 0.0 0.0 0.35 98.50 SILICOCARBONATITE 772 4.94 0.42 12.81 0.0 0.0 0.0 0.0 0.0 0.0 0.0 4.93 1.12 0.0 0.0 0.0 0.0 0.0 21.53 8.37 0.0 0.0 8.72 0.0 0.0 3.66 3.03 31.13 0.0 0.0 0.0 0.0 0.38 101.02 771 0.0 0.37 0.0 0.0 7.61 4.11 0.0 0.0 0.0 0.0 1.40 0.0 0.0 0.0 0.0 0.0 0.0 17.12 7.10 0.0 0.0 10.82 0.0 0.0 2.20 4.17 41.87 0.71 0.0 0.0 0.0 0.43 97.92 Note: For sample descriptions, see Table A-l. Alkalic norms were calculated using the method of LeBas (1973). 774 2.12 0.0 7.14 10.28 0.0 0.0 0.0 0.0 0.0 0.76 3.85 0.0 0.0 0.0 1.21 0.83 0.27 19.91 7.15 0.0 0.0 14.15 7.09 0.0 0.0 1.37 23.40 0.0 0.0 0.0 0.0 0.35 99.89 All samples are from drill core. The locations of the drillholes are shown on Figure 3 (Chart A). 66 Ref. No. Sample No. Ref. No. 837 CCM49 246.8-247.25 772 833 CCM49 324.75-325.1 771 832 CCM49 332.5-332.9 774 773 CCM6 140.0-140.4 Sample No. CCM6 131.8-132.2 CCM6 102.9-103.3 CCM6 141.4-141.65
TABLE A-4. CONTINUED. Ref. No. QZ CO OR AB LC KAL NEPH CAR NS AC TH GEH AKM FE-AK D. WO D. EN D. FS FO FA ANDR HM MT SPH PERV RU AP CC MGS FL ZR BAD H20 SUM 817 0.0 0.06 14.93 0.0 8.01 0.0 0.0 0.0 0.0 0.0 3.18 1.71 0.0 0.0 0.0 0.0 0.0 22.05 9.72 0.0 0.0 11.62 0.0 0.0 3.98 2.34 23.18 0.0 0.0 0.0 0.0 0.43 101.22 SILICOCARBONATITE 816 6.14 0.0 7.55 7.17 0.0 0.0 0.0 0.0 0.0 1.29 4.74 0.0 0.0 0.0 0.0 0.0 0.0 16.10 7.25 0.0 0.0 16.49 2.95 0.0 2.70 1.54 28.18 0.0 0.0 0.0 0.0 0.35 102.45 831 1.41 0.52 0.71 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.18 0.0 0.0 0.0 0.0 0.0 0.0 51.51 12.62 0.0 0.0 5.08 0.0 0.0 0.39 2.15 22.65 2.16 0.0 0.0 0.0 0.75 100.15 R. P. SAGE RAUHAUGITE 787 0.0 0.32 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 2.56 -1.96 0.0 -2.23 0.0 4.43 0.0 0.0 0.10 0.0 0.0 0.0 7.57 47.59 38.34 0.0 0.0 0.0 0.32 97.05 786 0.0 0.38 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.0 0.36 2.48 -2.20 -0.27 -2.16 0.56 5.00 0.0 0.0 0.03 0.0 0.0 0.0 2.18 54.19 39.04 0.0 0.0 0.0 0.41 100.00 Note: For sample descriptions, see Table A-l. Alkalic norms were calculated using the method of LeBas (1973). All samples are from drill core. The locations of the drillholes are shown on Figure 3 (Chart A). Ref. No. Sample No. Ref. No. Sample No. 817 CCM35 128.9-129.3 787 CCM9 515.85-516.2 816 CCM35 134.4-135.0 786 CCM9 409.95-410.6 831 CCM49 344.0-344.4 67
- Page 25 and 26: R. P. SAGE p. 116) as a mixture of
- Page 27 and 28: R. P. SAGE cores to magnesio-arfved
- Page 29 and 30: R. P. SAGE mined thickness. Sandvik
- Page 31 and 32: TABLE 2. STRATIGRAPHY OF OVERBURDEN
- Page 33 and 34: R. P. SAGE containing approximately
- Page 35 and 36: INTERNAL STRUCTURES R. P. SAGE The
- Page 37 and 38: Economic Geology The Cargill Townsh
- Page 39 and 40: R. P. SAGE Thoburn (1984) prepared
- Page 41 and 42: Appendix A Petrographic Description
- Page 43 and 44: R. P. SAGE Clinohumite is anhedral
- Page 45 and 46: R. P. SAGE with brown cores and red
- Page 47 and 48: R. P. SAGE hedral grains disseminat
- Page 49 and 50: R. P. SAGE pyroxene and occurs alon
- Page 51 and 52: R. P. SAGE grains disseminated thro
- Page 53 and 54: TABLE A-2. MAJOR ELEMENT ANALYSES (
- Page 55 and 56: TABLE A-2. CONTINUED. Ref. No. SiO2
- Page 57 and 58: TABLE A-2. CONTINUED. Ref. No. SiO2
- Page 59 and 60: R. P. SAGE TABLE A-3. TRACE ELEMENT
- Page 61 and 62: TABLE A-3. CONTINUED. Ref. No. Ag A
- Page 63 and 64: TABLE A-3. CONTINUED. Ref. No. Ag A
- Page 65 and 66: TABLE A-3. CONTINUED. Ref. No. Ag A
- Page 67 and 68: TABLE A-3. CONTINUED. Ref. No. Ag A
- Page 69 and 70: TABLE A-3. CONTINUED. Ref. No. Ag A
- Page 71 and 72: TABLE A-4. CONTINUED. Ref. No. QZ C
- Page 73 and 74: TABLE A-4. CONTINUED. Ref. No. QZ C
- Page 75: TABLE A-4. CONTINUED. Ref. No. QZ C
- Page 79 and 80: TABLE A-4. CONTINUED. Ref. No. QZ C
- Page 81 and 82: R.P. SAGE TABLE A-5. AVERAGE CHEMIC
- Page 83 and 84: Appendix B — Electron Microprobe
- Page 85 and 86: R.P. SAGE TABLE B-2. MICROPROBE MIN
- Page 87 and 88: R. P. SAGE TABLE B-3. MICROPROBE MI
- Page 89 and 90: TABLE B-5. MICROPROBE MINERAL ANALY
- Page 91 and 92: R. P. SAGE TABLE B-6. MICROPROBE MI
- Page 93 and 94: R. P. SAGE TABLE B-7. MICROPROBE MI
- Page 95 and 96: R. P. SAGE TABLE B-9. MICROPROBE MI
- Page 97 and 98: References Allen, C. 1972: The Petr
- Page 99 and 100: Index Aeromagnetic data, 7, 21, 24
- Page 101 and 102: Kinking Biotite, Rauhaugite, 18 Phl
- Page 103: Chart A — Cargill Carbonatite Com
CARBONATITE - ALKALIC ROCK COMPLEXES: CARGILL TOWNSHIP<br />
TABLE A-4. CONTINUED.<br />
Ref. No.<br />
QZ<br />
CO<br />
OR<br />
AB<br />
LC<br />
KAL<br />
NEPH<br />
CAR<br />
NS<br />
AC<br />
TH<br />
GEH<br />
AKM<br />
FE-AK<br />
D. WO<br />
D. EN<br />
D. FS<br />
FO<br />
FA<br />
ANDR<br />
HM<br />
MT<br />
SPH<br />
PERV<br />
RU<br />
AP<br />
CC<br />
MGS<br />
FL<br />
ZR<br />
BAD<br />
H2O<br />
SUM<br />
837<br />
0.95<br />
0.35<br />
0.47<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.78<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
2.70<br />
3.60<br />
0.0<br />
0.0<br />
1.70<br />
0.0<br />
0.0<br />
0.24<br />
6.72<br />
75.89<br />
4.01<br />
0.0<br />
0.0<br />
0.0<br />
0.47<br />
97.89<br />
SOVITE<br />
833<br />
2.24<br />
0.40<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
1.08<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.21<br />
3.04<br />
0.0<br />
0.0<br />
2.59<br />
0.0<br />
0.0<br />
0.29<br />
14.86<br />
64.43<br />
8.10<br />
0.0<br />
0.0<br />
0.0<br />
0.27<br />
97.51<br />
832<br />
0.0<br />
0.48<br />
0.57<br />
0.0<br />
0.43<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
1.26<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
2.93<br />
0.0<br />
0.0<br />
1.48<br />
0.0<br />
0.0<br />
0.18<br />
7.39<br />
79.34<br />
3.71<br />
0.0<br />
0.0<br />
0.0<br />
0.33<br />
98.10<br />
773<br />
0.0<br />
0.0<br />
2.47<br />
0.0<br />
11.65<br />
0.0<br />
3.27<br />
0.0<br />
0.0<br />
10.73<br />
1.33<br />
0.0<br />
0.0<br />
0.0<br />
4.54<br />
3.52<br />
0.52<br />
26.19<br />
4.31<br />
0.0<br />
0.0<br />
5.94<br />
2.38<br />
0.0<br />
0.0<br />
4.02<br />
17.27<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.35<br />
98.50<br />
SILICOCARBONATITE<br />
772<br />
4.94<br />
0.42<br />
12.81<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
4.93<br />
1.12<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
21.53<br />
8.37<br />
0.0<br />
0.0<br />
8.72<br />
0.0<br />
0.0<br />
3.66<br />
3.03<br />
31.13<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.38<br />
101.02<br />
771<br />
0.0<br />
0.37<br />
0.0<br />
0.0<br />
7.61<br />
4.11<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
1.40<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
17.12<br />
7.10<br />
0.0<br />
0.0<br />
10.82<br />
0.0<br />
0.0<br />
2.20<br />
4.17<br />
41.87<br />
0.71<br />
0.0<br />
0.0<br />
0.0<br />
0.43<br />
97.92<br />
Note: For sample descriptions, see Table A-l. Alkalic norms were calculated using the<br />
method <strong>of</strong> LeBas (1973).<br />
774<br />
2.12<br />
0.0<br />
7.14<br />
10.28<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.76<br />
3.85<br />
0.0<br />
0.0<br />
0.0<br />
1.21<br />
0.83<br />
0.27<br />
19.91<br />
7.15<br />
0.0<br />
0.0<br />
14.15<br />
7.09<br />
0.0<br />
0.0<br />
1.37<br />
23.40<br />
0.0<br />
0.0<br />
0.0<br />
0.0<br />
0.35<br />
99.89<br />
All samples are from drill core. The locations <strong>of</strong> the drillholes are shown on Figure 3 (Chart<br />
A).<br />
66<br />
Ref. No. Sample No. Ref. No.<br />
837 CCM49 246.8-247.25 772<br />
833 CCM49 324.75-325.1 771<br />
832 CCM49 332.5-332.9 774<br />
773 CCM6 140.0-140.4<br />
Sample No.<br />
CCM6 131.8-132.2<br />
CCM6 102.9-103.3<br />
CCM6 141.4-141.65
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