Cargill Township carbonatite complex, District of ... - Geology Ontario
Cargill Township carbonatite complex, District of ... - Geology Ontario
Cargill Township carbonatite complex, District of ... - Geology Ontario
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Introduction<br />
The <strong>Cargill</strong> <strong>Township</strong> Carbonatite Complex lies within the Kapuskasing Sub-<br />
province <strong>of</strong> the Superior Province <strong>of</strong> the Canadian Shield. The <strong>complex</strong> is one <strong>of</strong><br />
several that occur within this subprovince. The intrusion has been dated by K-Ar<br />
isotopic techniques at 1740 Ma (Gittins et al. 1967) and by U-Pb techniques at<br />
1907 4 Ma (S.T. Kwon, Department <strong>of</strong> <strong>Geology</strong>, University <strong>of</strong> California,<br />
Santa Barbara, California, personal communication, 1987). The <strong>carbonatite</strong><br />
<strong>complex</strong> has been emplaced along regional faults characteristic <strong>of</strong> the Kapuskas<br />
ing Subprovince and has been in turn <strong>of</strong>fset by later fault movements. This fault<br />
ing has split the <strong>complex</strong> into two parts so that it has a dumbbell shape in plan<br />
view with the long axis trending northeast. The body has been the subject <strong>of</strong><br />
several exploration programs culminating in 1974 with the discovery <strong>of</strong> residual<br />
apatite accumulations by the International Minerals and Chemical Corporation<br />
(Canada) Limited. The apatite deposits have potential economic significance as a<br />
source <strong>of</strong> phosphate.<br />
At the time <strong>of</strong> writing, Sherritt Gordon Mines Limited was undertaking addi<br />
tional work to evaluate the economic potential <strong>of</strong> the residual apatite deposits<br />
lying on the surface <strong>of</strong> the <strong>carbonatite</strong>.<br />
Acknowledgments<br />
The present study <strong>of</strong> the <strong>complex</strong> would not have been possible without the full<br />
cooperation <strong>of</strong> the International Minerals and Chemical Corporation (Canada)<br />
Limited. Mr. Ralph McGinn, in charge <strong>of</strong> operations at the property, guided the<br />
field party while visiting the property. Dr. George Erdosh, senior geologist, and<br />
Dr. P.O. Sandvik at the head <strong>of</strong>fice in Libertyville, Illinois, provided considerable<br />
support and encouragement to the project. All samples described were obtained<br />
from diamond drill core <strong>of</strong> the International Minerals and Chemical Corporation.<br />
In 1976, Mr. Wilbur Wright, senior geological assistant, examined approxi<br />
mately half the core sampled by the field party. Mr. Paul Chamois and Mr. Carl<br />
Higgins served as geological assistants, helping both the author and Mr. Wright in<br />
sampling. Mr. A. Lisowyk, geological assistant, recalculated statistics on whole-<br />
rock chemistry and revised the tables in Appendix A in 1988.<br />
Mr. H.L. Banting, Continental Copper Mines Limited, gave approval to Ken-<br />
nco Exploration (Canada) Limited to release to the Ministry data concerning<br />
Kennco's work on the <strong>complex</strong>. Mr. H.W. Fleming, chief geologist, Kennco Ex<br />
ploration (Canada) Limited released the data to the Ministry.<br />
Mr. Gary Hughes, Exploration Manager, Sherritt Gordon Mines Limited,<br />
provided the <strong>Ontario</strong> Geological Survey with data obtained by that company re<br />
sulting from its work on the <strong>complex</strong>. In 1981, Mr. L. Kelley, geologist, Sherritt<br />
Gordon Mines Limited, guided the author during operations to uncover the resid<br />
ual apatite deposits for the purpose <strong>of</strong> bulk sampling.<br />
In 1987, Mr. B. Hystead, Manager, Mineral Resource Development, Sherritt<br />
Gordon Mines Limited, Mr. L. Kelley, geologist, Sherritt Gordon Mines Limited,<br />
and Mr. P. Potap<strong>of</strong>f, senior geologist, Camchib Resources Limited, provided re<br />
ports and data resulting from exploration efforts since 1981.<br />
Location And Access<br />
The <strong>Cargill</strong> <strong>Township</strong> Carbonatite Complex is located at approximately 49 0 19'N<br />
Latitude and 82 0 49'W Longitude (Figure 1) in the northwest corner <strong>of</strong> <strong>Cargill</strong>