Zobrazeno 1 - 8
of 8
pro vyhledávání: '"John S. Fedorowich"'
Publikováno v:
Economic Geology. 101:1595-1603
A geologic problem has been addressed in the Fraser-Strathcona Deep Copper mine, Sudbury, wherein diabase dikes and the chalcopyrite vein system have a mutually crosscutting relationship. In any situation where crosscutting relationships are mutual t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::174ab3f9c5e2973d96b1af3369628694
https://doi.org/10.2113/gsecongeo.101.8.1595
https://doi.org/10.2113/gsecongeo.101.8.1595
Publikováno v:
The Canadian Mineralogist. 44:1063-1077
La mine Thayer Lindsley, situee sur le flanc sud du complexe igne de Sudbury (1.85 Ga), fournit un exemple d'une mineralisation en sulfures de Ni-Cu-EGP pres du contact et en sulfures de Cu-Ni-EGP dans la paroi inferieure (EGP: elements du groupe du
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::11a7ade1e6c278a38581bfa7191f8ef6
https://doi.org/10.2113/gscanmin.44.5.1063
https://doi.org/10.2113/gscanmin.44.5.1063
Autor:
Joshua Bailey, Andrew M. McDonald, Douglas A. Archibald, John S. Fedorowich, Bruno Lafrance, Sandra L. Kamo
Publikováno v:
Canadian Journal of Earth Sciences. 41:1491-1505
The Thayer Lindsley mine is located in the South Range of the Sudbury impact structure, near the contact between the 1.85 Ga Sudbury Igneous Complex (SIC) and the Paleoproterozoic Southern Province. NiCu ore zones at the mine are strongly deformed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a447e84023808bd890056ead301455be
https://doi.org/10.1139/e04-098
https://doi.org/10.1139/e04-098
Publikováno v:
Canadian Journal of Earth Sciences. 40:1009-1025
The Needle Falls Shear Zone is a major Paleoproterozoic discontinuity separating an Archean craton from accreted Paleoproterozoic terranes in the western Trans-Hudson Orogen. It is a 1 km-wide subvertical mylonite zone forming the southwestern sector
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e50d502f2d2a23e0a9d32e7ec0d444d1
https://doi.org/10.1139/e03-033
https://doi.org/10.1139/e03-033
Publikováno v:
Earth-Science Reviews. 60:147-174
The Sudbury Structure, formed by meteorite impact at 1850 Ma, consists of three major components: (1) the Sudbury Basin; (2) the Sudbury Igneous Complex, which surrounds the basin as an elliptical collar; and (3) breccia bodies in the footwall known
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4d85f56ee5776247ae40ffbe38faf0fd
https://doi.org/10.1016/s0012-8252(02)00091-0
https://doi.org/10.1016/s0012-8252(02)00091-0
Publikováno v:
Chemical Geology. 106:229-249
A new method of producing glass beads from whole-rock powders has been tested for use in laser sampling-inductively coupled plasma-mass spectrometry (LS-ICP-MS). Glass beads are produced in a tungsten strip heater cell, under an Ar atmosphere of 275
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::932cc4501b4c16c8496a5f87304979a5
https://doi.org/10.1016/0009-2541(93)90029-i
https://doi.org/10.1016/0009-2541(93)90029-i
Publikováno v:
Economic Geology. 86:1434-1467
The late-kinematic structural architecture of the Flin Flon domain is dominated by a network of anastomosing shear zones formed by compressional deformation during the Proterozoic Trans-Hudson orogeny (ca. 1900-1800 Ma). A number of structurally cont
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec06b36974f0f9021ba4eaddffae376f
https://doi.org/10.2113/gsecongeo.86.7.1434
https://doi.org/10.2113/gsecongeo.86.7.1434
