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pro vyhledávání: '"M. D. Thomas"'
Autor:
M D Thomas
Differences of opinion concerning the relationship between the Thelon tectonic zone and the Taltson magmatic zone, as to whether they are individual tectonic elements or two independent elements, have generated various plate tectonic models explainin
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https://explore.openaire.eu/search/publication?articleId=doi_________::cb13c54497f61525fdc39161dda3aeef
https://doi.org/10.4095/329250
https://doi.org/10.4095/329250
Autor:
M D Thomas
A prominent magnetic low along an eastern portion of the Paleoproterozoic Taltson magmatic zone (TMZ) correlates mainly with the youngest granitoid in the zone, the peraluminous ca. 1936 Ma Konth granite. Flanking belts of higher magnetic intensity c
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https://explore.openaire.eu/search/publication?articleId=doi_________::d3a36529cf67d0fa7c88b03b25977b71
https://doi.org/10.4095/328244
https://doi.org/10.4095/328244
Publikováno v:
Canadian Journal of Earth Sciences. 56:452-470
An airborne gravity gradiometer survey was recently flown over the Iron Range Fault in the Purcell anticlinorium, southern Canadian Cordillera. The fault is commonly associated with iron oxide mineralization having characteristics similar to those of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0dda9360565a507b0a1f48ad80c6f1e2
https://doi.org/10.1139/cjes-2018-0047
https://doi.org/10.1139/cjes-2018-0047
Akademický článek
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Autor:
M. D. Thomas
Publikováno v:
Canadian Journal of Earth Sciences. 52:368-385
Two-dimensional magnetic models of the Moyie anticline contribute to an independent project targeting development of a regional three-dimensional (3D) model of much of the Purcell anticlinorium by compensating for shortcomings in reflection seismic s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::792b83c864fdb69ffcc8d0fec37e9c98
https://doi.org/10.1139/cjes-2014-0224
https://doi.org/10.1139/cjes-2014-0224