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-3. CONTINUED. Ref. No. Ag Au As Ba Be Bi Co Cr Cu Ga Hg Li Mn Mo Nb Ni Pb Rb Sb Se Sn Sr Ti V Y Zn Zr La Nd Ce Yb Eu 824 1 30 *C1 110 1060 1500 10 O -Ci oo 680 25 •CIO 45 4 150 600 10 85 85 •O 00 ^00 430 2 ^00 823 •O 70 ^ 120 780 690 9 O 2 00 500 20 •CIO 35 3 60 600 10 120 120 ^00 •ci 00 350 2 •Ci 00 PYROXENITE 822 •CI 20 •CI 125 660 630 10 3 1 OO 480 •CIO •CIO 40 3 60 700 10 120 120 ^00 •CI 00 380 2 •CI 00 819 •ci 140 •Ci 80 680 500 15 0 •0 OO 135 20 •CIO 40 4 200 400 10 100 200 •Ci 00 •Ci 00 660 1 •C100 830 •CI 50
TABLE A-3. CONTINUED. Ref. No. Ag Au As Ba Be Bi Co Cr Cu Ga Hg Li Mn Mo Nb Ni Pb Rb Sb Se Sn Sr Ti V Y Zn Zr La Nd Ce Yb Eu 840 60 100 1060 920 7 oo 580 20 45 O 250 300 15 95 100 ^00 ^00 200 1 •ci 00 R. P. SAGE PYROXENITE MISCELLANEOUS 841 60 90 1180 500 7 OO 400 15 50 O 200 350 10 90 100 •CI 00 •C100 200 1 •ci 00 842 50 55 1900 250 4 O OO 310 10 •CIO 60 O 150 200 10 50 60 ^00 *:100 180 *C1 •C100 843 •Ci 80 135 620 640 20 7 OO 440 •CIO •CIO 30 4 150 700 10 160 100 ^00 *aOO 510 2 •CI 00 815 •ci 410 •CI 105 75 125 25 O 30 140 15 20 30 10 300 500 10 180 300 •CI 00 •C100 940 3 •ci 00 818 •Ci 470 15 30 85 80 15 •ci 150 25 15 30 20 7 700 400 25 85 300 •C100
- Page 17 and 18: General Geology The Cargill Townshi
- Page 19 and 20: R. P. SAGE A crandallite-rich blank
- Page 21 and 22: R. P. SAGE more euhedral when in co
- Page 23 and 24: Other Mafic to Ultramafic Rocks R.
- 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: 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 and 76: TABLE A-4. CONTINUED. Ref. No. QZ C
- Page 77 and 78: 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
TABLE A-3. CONTINUED.<br />
Ref. No.<br />
Ag<br />
Au<br />
As<br />
Ba<br />
Be<br />
Bi<br />
Co<br />
Cr<br />
Cu<br />
Ga<br />
Hg<br />
Li<br />
Mn<br />
Mo<br />
Nb<br />
Ni<br />
Pb<br />
Rb<br />
Sb<br />
Se<br />
Sn<br />
Sr<br />
Ti<br />
V<br />
Y<br />
Zn<br />
Zr<br />
La<br />
Nd<br />
Ce<br />
Yb<br />
Eu<br />
840<br />
60<br />
100<br />
1060<br />
920<br />
7<br />
oo<br />
580<br />
20<br />
45<br />
O<br />
250<br />
300<br />
15<br />
95<br />
100<br />
^00<br />
^00<br />
200<br />
1<br />
•ci 00<br />
R. P. SAGE<br />
PYROXENITE MISCELLANEOUS<br />
841<br />
60<br />
90<br />
1180<br />
500<br />
7<br />
OO<br />
400<br />
15<br />
50<br />
O<br />
200<br />
350<br />
10<br />
90<br />
100<br />
•CI 00<br />
•C100<br />
200<br />
1<br />
•ci 00<br />
842<br />
50<br />
55<br />
1900<br />
250<br />
4<br />
O<br />
OO<br />
310<br />
10<br />
•CIO<br />
60<br />
O<br />
150<br />
200<br />
10<br />
50<br />
60<br />
^00<br />
*:100<br />
180<br />
*C1<br />
•C100<br />
843<br />
•Ci<br />
80<br />
135<br />
620<br />
640<br />
20<br />
7<br />
OO<br />
440<br />
•CIO<br />
•CIO<br />
30<br />
4<br />
150<br />
700<br />
10<br />
160<br />
100<br />
^00<br />
*aOO<br />
510<br />
2<br />
•CI 00<br />
815<br />
•ci<br />
410<br />
•CI<br />
105<br />
75<br />
125<br />
25<br />
O<br />
30<br />
140<br />
15<br />
20<br />
30<br />
10<br />
300<br />
500<br />
10<br />
180<br />
300<br />
•CI 00<br />
•C100<br />
940<br />
3<br />
•ci 00<br />
818<br />
•Ci<br />
470<br />
15<br />
30<br />
85<br />
80<br />
15<br />
•ci<br />
150<br />
25<br />
15<br />
30<br />
20<br />
7<br />
700<br />
400<br />
25<br />
85<br />
300<br />
•C100<br />
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