Zobrazeno 1 - 10 of 22 pro vyhledávání: '"Frederick M. Haynes"'
2
Relation of mineralization to wall-rock alteration and brecciation, Mascot-Jefferson City mississippi valley-type district, Tennessee
Autor: Stephen E. Kesler, Frederick M. Haynes
Publikováno v: Economic Geology. 89:51-66
This study was undertaken to assess the relation of Mississippi Valley-type mineralization to wall-rock alteration and brecciation in the Mascot-Jefferson City district, the largest part of the East Tennessee Mississippi Valley-type ore field. The ma
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a46af9fd78151a79beea71e7e57670c5
https://doi.org/10.2113/gsecongeo.89.1.51
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4
Fluid inclusion chemistry in the exploration for Mississippi Valley-type deposits: an example from East Tennessee, U.S.A
Autor: Frederick M. Haynes, Stephen E. Kesler
Publikováno v: Applied Geochemistry. 2:321-327
Scanning electron microscopy and energy dispersive analysis of fluid inclusion decrepitates in sparry dolomite cements associated with sphalerite mineralization in the Mascot-Jefferson City Missis- sippi Valley-type district of East Tennessee show a
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::3844635b529cf17c0a1807ffdef87c80
https://doi.org/10.1016/0883-2927(87)90047-3
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6
Late Paleozoic magnetization of mineralized and unmineralized ordovician carbonates from east Tennessee: Evidence for a post-ore chemical event
Autor: Rob Van der Voo, Frederick M. Haynes, Valerian Bachtadse, Stephen E. Kesler
Publikováno v: Journal of Geophysical Research: Solid Earth. 92:14165-14176
Thermal demagnetization studies on samples from mineralized and unmineralized rocks in the Lower Ordovician Knox Group of east Tennessee reveal a mean direction of D/I = 157°/+18° (α95 = 7.7°, k = 52.9) after 60% unfolding, combining stable endpo
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b9401245a57f4d0acdb361f7ea128a53
https://doi.org/10.1029/jb092ib13p14165
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7
Fluid-inclusion evidence of basinal brines in Archean basement, Thunder Bay Pb–Zn–Ba district, Ontario, Canada
Autor: Frederick M. Haynes
Publikováno v: Canadian Journal of Earth Sciences. 25:1884-1894
Fluid inclusions from three quartz–galena–sphalerite–barite–calcite veins in the Thunder Bay district of western Ontario contain liquid + vapor ± halite and homogenize by vapor disappearance or halite dissolution at temperatures of 90–200
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5c3bce079d3dd18735031a9d39fe60e0
https://doi.org/10.1139/e88-177
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8
Chemical evolution of brines during mississippi valley-type mineralization; evidence from East Tennessee and Pine Point
Autor: Stephen E. Kesler, Frederick M. Haynes
Publikováno v: Economic Geology. 82:53-71
The major element chemical composition of inclusion fluids from Mississippi Valley-type deposits has been evaluated semiquantitatively using scanning electron microscopy and energy dispersive analysis of individual inclusion decrepitates in ore and g
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a8336b62821e1896a854706631dbefc1
https://doi.org/10.2113/gsecongeo.82.1.53
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